Évolution géodynamique de l'Indonésie orientale, de l'Éocène au Pliocène
Identifieur interne : 001638 ( Istex/Corpus ); précédent : 001637; suivant : 001639Évolution géodynamique de l'Indonésie orientale, de l'Éocène au Pliocène
Auteurs : Michel Villeneuve ; Jean-Pierre Réhault ; Jean-Jacques Cornée ; Christian Honthaas ; Wahyu Gunawan CSource :
- Comptes Rendus de l'Academie des Sciences Series IIA Earth and Planetary Science [ 1251-8050 ] ; 1998.
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Abstract
Abstract: Eastern Indonesia belongs to a convergent zone between the Asiatic, Australian and Pacific plates. A lot of synthetic papers have been devoted to this very technically active area. Our new geodynamic reconstruction takes into account a six year period of scientific cooperation between France and Indonesia. This cooperation provided various geological data. The hypothesis presented here is based on the geological evolution of lour small commentai blocks (two of which appear for the first time: the Banda und l.ucipara blocks) trapped by the convergence of the threemain plates. The main steps are successively: the Upper Eocene to Oligocene. during which the Banda block collided with the south east asiatic margin in Sulawesi: the Lower Miocene, during which the l.iicipara block (including (he Tukang IJesi platform) collided with the Banda block itself, mainly in the Buton area: the Upper Miocene, which is a period of large extensional regime. Most of the basins inside the Banda area opened at that time (North Banda Basin, South Banda Basin, Savu Basin, etc.). The next interesting period is the Upper Pliocene, which occurred after the main collisions between the Australian continental block and the Banda and Irian Java blocks. The Bangai Sula block collided with the eastern part of Sulawesi at the end of the Lower Pliocene.
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DOI: 10.1016/S1251-8050(98)80046-3
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Le-Gorgeu, 29285 Brost cedex, France</mods:affiliation></affiliation></author><author><name sortKey="Cornee, Jean Jacques" sort="Cornee, Jean Jacques" uniqKey="Cornee J" first="Jean-Jacques" last="Cornée">Jean-Jacques Cornée</name><affiliation><mods:affiliation>Centre de sédimentologie et paléontologie, Upresa 6019, CNRS et université de Provence, case 67, 3, place Victor-Hugo, 13331 Marseille cedex 03, France</mods:affiliation></affiliation></author><author><name sortKey="Honthaas, Christian" sort="Honthaas, Christian" uniqKey="Honthaas C" first="Christian" last="Honthaas">Christian Honthaas</name><affiliation><mods:affiliation>Géophysique marine, UBO, BP 239, 6, av. Le-Gorgeu, 29285 Brost cedex, France</mods:affiliation></affiliation></author><author><name sortKey="Gunawan C, Wahyu" sort="Gunawan C, Wahyu" uniqKey="Gunawan C W" first="Wahyu" last="Gunawan C">Wahyu Gunawan C</name></author></analytic><monogr></monogr><series><title level="j">Comptes Rendus de l'Academie des Sciences Series IIA Earth and Planetary Science</title><title level="j" type="abbrev">PXTOLD</title><idno type="ISSN">1251-8050</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1998">1998</date><biblScope unit="volume">327</biblScope><biblScope unit="issue">5</biblScope><biblScope unit="page" from="291">291</biblScope><biblScope unit="page" to="302">302</biblScope></imprint><idno type="ISSN">1251-8050</idno></series><idno type="istex">79143E3277C8F236120CC1CEC0B1B207B43043E8</idno><idno type="DOI">10.1016/S1251-8050(98)80046-3</idno><idno type="PII">S1251-8050(98)80046-3</idno><idno type="ArticleID">98800463</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">1251-8050</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Australia</term><term>Australie</term><term>Eocene</term><term>Indonesia</term><term>Indonésie</term><term>Miocene</term><term>Miocène</term><term>Oligocene</term><term>Oligocène</term><term>Pliocène</term><term>Pllocene</term><term>arcs volcaniques</term><term>basin openings</term><term>collisions</term><term>geodynamic reconstructions</term><term>ouverture de bassins</term><term>reconstructions géodynamiques</term><term>volcanic arcs</term><term>Éocène</term></keywords></textClass><langUsage><language ident="fr">fr</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Eastern Indonesia belongs to a convergent zone between the Asiatic, Australian and Pacific plates. A lot of synthetic papers have been devoted to this very technically active area. Our new geodynamic reconstruction takes into account a six year period of scientific cooperation between France and Indonesia. This cooperation provided various geological data. The hypothesis presented here is based on the geological evolution of lour small commentai blocks (two of which appear for the first time: the Banda und l.ucipara blocks) trapped by the convergence of the threemain plates. The main steps are successively: the Upper Eocene to Oligocene. during which the Banda block collided with the south east asiatic margin in Sulawesi: the Lower Miocene, during which the l.iicipara block (including (he Tukang IJesi platform) collided with the Banda block itself, mainly in the Buton area: the Upper Miocene, which is a period of large extensional regime. Most of the basins inside the Banda area opened at that time (North Banda Basin, South Banda Basin, Savu Basin, etc.). The next interesting period is the Upper Pliocene, which occurred after the main collisions between the Australian continental block and the Banda and Irian Java blocks. The Bangai Sula block collided with the eastern part of Sulawesi at the end of the Lower Pliocene.</div></front></TEI><istex><corpusName>elsevier</corpusName><author><json:item><name>Michel Villeneuve</name><affiliations><json:string>Centre de sédimentologie et paléontologie, Upresa 6019, CNRS et université de Provence, case 67, 3, place Victor-Hugo, 13331 Marseille cedex 03, France</json:string><json:string>E-mail: mville@newsup.univ-mrs.fr</json:string></affiliations></json:item><json:item><name>Jean-Pierre Réhault</name><affiliations><json:string>Géophysique marine, UBO, BP 239, 6, av. Le-Gorgeu, 29285 Brost cedex, France</json:string></affiliations></json:item><json:item><name>Jean-Jacques Cornée</name><affiliations><json:string>Centre de sédimentologie et paléontologie, Upresa 6019, CNRS et université de Provence, case 67, 3, place Victor-Hugo, 13331 Marseille cedex 03, France</json:string></affiliations></json:item><json:item><name>Christian Honthaas</name><affiliations><json:string>Géophysique marine, UBO, BP 239, 6, av. Le-Gorgeu, 29285 Brost cedex, France</json:string></affiliations></json:item><json:item><name>Wahyu Gunawan c</name></json:item></author><subject><json:item><lang><json:string>fre</json:string></lang><value>Le point sur…</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Indonésie</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Australie</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>reconstructions géodynamiques</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>arcs volcaniques</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>ouverture de bassins</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>collisions</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Éocène</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Oligocène</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Miocène</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Pliocène</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Indonesia</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Australia</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>geodynamic reconstructions</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>volcanic arcs</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>basin openings</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>collisions</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Eocene</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Oligocene</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Miocene</value></json:item><json:item><lang><json:string>fre</json:string></lang><value>Pllocene</value></json:item></subject><articleId><json:string>98800463</json:string></articleId><language><json:string>fre</json:string></language><originalGenre><json:string>Review article</json:string></originalGenre><abstract>Abstract: Eastern Indonesia belongs to a convergent zone between the Asiatic, Australian and Pacific plates. A lot of synthetic papers have been devoted to this very technically active area. Our new geodynamic reconstruction takes into account a six year period of scientific cooperation between France and Indonesia. This cooperation provided various geological data. The hypothesis presented here is based on the geological evolution of lour small commentai blocks (two of which appear for the first time: the Banda und l.ucipara blocks) trapped by the convergence of the threemain plates. The main steps are successively: the Upper Eocene to Oligocene. during which the Banda block collided with the south east asiatic margin in Sulawesi: the Lower Miocene, during which the l.iicipara block (including (he Tukang IJesi platform) collided with the Banda block itself, mainly in the Buton area: the Upper Miocene, which is a period of large extensional regime. Most of the basins inside the Banda area opened at that time (North Banda Basin, South Banda Basin, Savu Basin, etc.). The next interesting period is the Upper Pliocene, which occurred after the main collisions between the Australian continental block and the Banda and Irian Java blocks. The Bangai Sula block collided with the eastern part of Sulawesi at the end of the Lower Pliocene.</abstract><qualityIndicators><score>7.114</score><pdfVersion>1.3</pdfVersion><pdfPageSize>612.08 x 791.96 pts (letter)</pdfPageSize><refBibsNative>true</refBibsNative><keywordCount>21</keywordCount><abstractCharCount>1350</abstractCharCount><pdfWordCount>4558</pdfWordCount><pdfCharCount>43332</pdfCharCount><pdfPageCount>12</pdfPageCount><abstractWordCount>213</abstractWordCount></qualityIndicators><title>Évolution géodynamique de l'Indonésie orientale, de l'Éocène au Pliocène</title><pii><json:string>S1251-8050(98)80046-3</json:string></pii><corporate><json:item><name>le groupe Géobanda</name></json:item></corporate><refBibs><json:item><host><author></author><title>Preliminary geological map of Kai (and Tual) Quadrangles, Maluku, Scale 1:250 000</title></host></json:item><json:item><author><json:item><name>J.R. Ali</name></json:item><json:item><name>J. 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Le-Gorgeu, 29285 Brost cedex, France</affiliation></author><author xml:id="author-4"><persName><forename type="first">Jean-Jacques</forename><surname>Cornée</surname></persName><affiliation>Centre de sédimentologie et paléontologie, Upresa 6019, CNRS et université de Provence, case 67, 3, place Victor-Hugo, 13331 Marseille cedex 03, France</affiliation></author><author xml:id="author-5"><persName><forename type="first">Christian</forename><surname>Honthaas</surname></persName><affiliation>Géophysique marine, UBO, BP 239, 6, av. Le-Gorgeu, 29285 Brost cedex, France</affiliation></author><author xml:id="author-6"><persName><forename type="first">Wahyu</forename><surname>Gunawan c</surname></persName></author></analytic><monogr><title level="j">Comptes Rendus de l'Academie des Sciences Series IIA Earth and Planetary Science</title><title level="j" type="abbrev">PXTOLD</title><idno type="pISSN">1251-8050</idno><idno type="PII">S1251-8050(00)X0092-4</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1998"></date><biblScope unit="volume">327</biblScope><biblScope unit="issue">5</biblScope><biblScope unit="page" from="291">291</biblScope><biblScope unit="page" to="302">302</biblScope></imprint></monogr><idno type="istex">79143E3277C8F236120CC1CEC0B1B207B43043E8</idno><idno type="DOI">10.1016/S1251-8050(98)80046-3</idno><idno type="PII">S1251-8050(98)80046-3</idno><idno type="ArticleID">98800463</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1998</date></creation><langUsage><language ident="fr">fr</language></langUsage><abstract xml:lang="en"><p>Abstract: Eastern Indonesia belongs to a convergent zone between the Asiatic, Australian and Pacific plates. A lot of synthetic papers have been devoted to this very technically active area. Our new geodynamic reconstruction takes into account a six year period of scientific cooperation between France and Indonesia. This cooperation provided various geological data. The hypothesis presented here is based on the geological evolution of lour small commentai blocks (two of which appear for the first time: the Banda und l.ucipara blocks) trapped by the convergence of the threemain plates. The main steps are successively: the Upper Eocene to Oligocene. during which the Banda block collided with the south east asiatic margin in Sulawesi: the Lower Miocene, during which the l.iicipara block (including (he Tukang IJesi platform) collided with the Banda block itself, mainly in the Buton area: the Upper Miocene, which is a period of large extensional regime. Most of the basins inside the Banda area opened at that time (North Banda Basin, South Banda Basin, Savu Basin, etc.). The next interesting period is the Upper Pliocene, which occurred after the main collisions between the Australian continental block and the Banda and Irian Java blocks. The Bangai Sula block collided with the eastern part of Sulawesi at the end of the Lower Pliocene.</p></abstract><abstract xml:lang="fr"><p>Résumé: L'Indonésie orientale correspond á la zone de convergence entre trois grandes plaques: Asiatique, Australienne et Pacifique. De nombreuses synthèses ont vu le jour sur cette zone particulièrement active. Nous proposons ici une nouvelle hypothèse sur Article rédigé à l'attention du Comité de lecture. Article remis le 30 mars 1998, accepté après révision le 3 août 1998. l'évolution géodynamique. Elle tient compte des nombreuses observations effectuées tant à terre qu'en mer (depuis 1989) r des équipes franco-indonésiennes. Cette hypothèse rend compte de la présence de quatre blocs de petite taille (dont deux individualisés pour la première fois: blocs de Banda et de Lucipara) qui se sont trouvés ≪ coincés ≫ entre les trois grandes plaques. Nous donnons la composition des differents blocs et leur cheminement au travers des reconstitutions paléogéographiques pour quatre périodes clés de l'évolution géologique de ette zone. Ces périodes sont: l'Éocène supérieur à l'Oligocène supérieur, au cours duquel le bloc de Banda s'est accrété à la mrge asiatique, le Miocène inférieur,au cours duquel le bloc de Lucipara est entré en collision avec le bloc de Banda, le Miocène supérieur, qui est la grande période d'extension au cours de laquelle se sont formés les principaux bassins entourés par l'arc de Banda, et le Pliocène supérieur, qui succède à la collision entre le continent australien et l'arc de Banda d'une part et lrian Jaya, d'autre part.</p></abstract><textClass><keywords scheme="keyword"><list><head>article-category</head><item><term>Le point sur…</term></item></list></keywords></textClass><textClass xml:lang="en"><keywords scheme="keyword"><list><item><term>Indonésie</term></item><item><term>Australie</term></item><item><term>reconstructions géodynamiques</term></item><item><term>arcs volcaniques</term></item><item><term>ouverture de bassins</term></item><item><term>collisions</term></item><item><term>Éocène</term></item><item><term>Oligocène</term></item><item><term>Miocène</term></item><item><term>Pliocène</term></item></list></keywords></textClass><textClass xml:lang="en"><keywords scheme="keyword"><list><item><term>Indonesia</term></item><item><term>Australia</term></item><item><term>geodynamic reconstructions</term></item><item><term>volcanic arcs</term></item><item><term>basin openings</term></item><item><term>collisions</term></item><item><term>Eocene</term></item><item><term>Oligocene</term></item><item><term>Miocene</term></item><item><term>Pllocene</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1998">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/79143E3277C8F236120CC1CEC0B1B207B43043E8/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Elsevier doc found" wicri:toSee="Elsevier, no converted or simple article"><istex:xmlDeclaration>version="1.0" encoding="utf-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//ES//DTD journal article DTD version 5.0.1//EN//XML" URI="art501.dtd" name="istex:docType"></istex:docType><istex:document><article version="5.0" xml:lang="fr" docsubtype="rev"><item-info><jid>PXTOLD</jid><aid>98800463</aid><ce:pii>S1251-8050(98)80046-3</ce:pii><ce:doi>10.1016/S1251-8050(98)80046-3</ce:doi><ce:copyright type="unknown" year="1998">Académie des sciences/Elsevier, Paris</ce:copyright><ce:doctopics><ce:doctopic><ce:text>Le point sur…</ce:text><ce:doctopic><ce:text>Géodynamique</ce:text></ce:doctopic></ce:doctopic></ce:doctopics></item-info><head><ce:dochead><ce:textfn>Concise review paper</ce:textfn></ce:dochead><ce:title>Évolution géodynamique de l'Indonésie orientale, de l'Éocène au Pliocène</ce:title><ce:alt-title xml:lang="en">Geodynamic evolution of Eastern Indonesia from the Eocene to the Pliocene</ce:alt-title><ce:author-group><ce:author><ce:given-name>Michel</ce:given-name><ce:surname>Villeneuve</ce:surname><ce:cross-ref refid="aff1"><ce:sup>a</ce:sup></ce:cross-ref><ce:e-address type="email">mville@newsup.univ-mrs.fr</ce:e-address></ce:author><ce:author><ce:given-name>Jean-Pierre</ce:given-name><ce:surname>Réhault</ce:surname><ce:cross-ref refid="aff2"><ce:sup>b</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Jean-Jacques</ce:given-name><ce:surname>Cornée</ce:surname><ce:cross-ref refid="aff1"><ce:sup>a</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Christian</ce:given-name><ce:surname>Honthaas</ce:surname><ce:cross-ref refid="aff2"><ce:sup>b</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Wahyu</ce:given-name><ce:surname>Gunawan c</ce:surname></ce:author><ce:collaboration><ce:text>le groupe Géobanda</ce:text><ce:cross-ref refid="fn1"><ce:sup>**</ce:sup></ce:cross-ref></ce:collaboration><ce:affiliation id="aff1"><ce:label>a</ce:label><ce:textfn>Centre de sédimentologie et paléontologie, Upresa 6019, CNRS et université de Provence, case 67, 3, place Victor-Hugo, 13331 Marseille cedex 03, France</ce:textfn></ce:affiliation><ce:affiliation id="aff2"><ce:label>b</ce:label><ce:textfn>Géophysique marine, UBO, BP 239, 6, av. Le-Gorgeu, 29285 Brost cedex, France</ce:textfn></ce:affiliation><ce:affiliation id="aff3"><ce:label>c</ce:label><ce:textfn>GRDC, lalan Diponegoro 57, 40122, Bandung, Indonésie</ce:textfn></ce:affiliation><ce:footnote id="fn1"><ce:label>**</ce:label><ce:note-para>Le groupe Geobanda comprend: Y. Anantasema (BBPT, Jakarta), H. Bellon (Géosciences Brest), S. Burhanuddin (université de Sulawesi, Ujung Pandang, Indonésie), J. Butterlin (IPGP, Paris), J. Clermonté, (Géologie, Nancy), J. Girardeau (Pétrologie, Nantes), A.H. Harsolumakso (Geology, ITB, Bandung, Indonésie), B. Lathuillère (Géologie, Nancy), J.-A. Malod (Géophysique Marine, Brest), C. Monnier (Pétrologie, Nantes), L. Sarmili (MGI, Bandung, Indonésie), P. Saint-Marc (Géosciences Azur, Sophia-Antipolis) et C. Tronchetti (Géologie, Marseille).</ce:note-para></ce:footnote></ce:author-group><ce:abstract id="ab1" class="author" xml:lang="en"><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para>Eastern Indonesia belongs to a convergent zone between the Asiatic, Australian and Pacific plates. A lot of synthetic papers have been devoted to this very technically active area. Our new geodynamic reconstruction takes into account a six year period of scientific cooperation between France and Indonesia. This cooperation provided various geological data. The hypothesis presented here is based on the geological evolution of lour small commentai blocks (two of which appear for the first time: the Banda und l.ucipara blocks) trapped by the convergence of the threemain plates. The main steps are successively: the Upper Eocene to Oligocene. during which the Banda block collided with the south east asiatic margin in Sulawesi: the Lower Miocene, during which the l.iicipara block (including (he Tukang IJesi platform) collided with the Banda block itself, mainly in the Buton area: the Upper Miocene, which is a period of large extensional regime. Most of the basins inside the Banda area opened at that time (North Banda Basin, South Banda Basin, Savu Basin, etc.). The next interesting period is the Upper Pliocene, which occurred after the main collisions between the Australian continental block and the Banda and Irian Java blocks. The Bangai Sula block collided with the eastern part of Sulawesi at the end of the Lower Pliocene.</ce:simple-para></ce:abstract-sec></ce:abstract><ce:abstract id="ab2" class="author" xml:lang="fr"><ce:section-title>Résumé</ce:section-title><ce:abstract-sec><ce:simple-para>L'Indonésie orientale correspond á la zone de convergence entre trois grandes plaques: Asiatique, Australienne et Pacifique. De nombreuses synthèses ont vu le jour sur cette zone particulièrement active. Nous proposons ici une nouvelle hypothèse sur Article rédigé à l'attention du Comité de lecture. Article remis le 30 mars 1998, accepté après révision le 3 août 1998. l'évolution géodynamique. Elle tient compte des nombreuses observations effectuées tant à terre qu'en mer (depuis 1989) r des équipes franco-indonésiennes. Cette hypothèse rend compte de la présence de quatre blocs de petite taille (dont deux individualisés pour la première fois: blocs de Banda et de Lucipara) qui se sont trouvés ≪ coincés ≫ entre les trois grandes plaques. Nous donnons la composition des differents blocs et leur cheminement au travers des reconstitutions paléogéographiques pour quatre périodes clés de l'évolution géologique de ette zone. Ces périodes sont: <ce:italic>l'Éocène supérieur à l'Oligocène supérieur</ce:italic>, au cours duquel le bloc de Banda s'est accrété à la mrge asiatique, le <ce:italic>Miocène inférieur</ce:italic>,au cours duquel le bloc de Lucipara est entré en collision avec le bloc de Banda, le <ce:italic>Miocène supérieur</ce:italic>, qui est la grande période d'extension au cours de laquelle se sont formés les principaux bassins entourés par l'arc de Banda, et le <ce:italic>Pliocène supérieur</ce:italic>, qui succède à la collision entre le continent australien et l'arc de Banda d'une part et lrian Jaya, d'autre part.</ce:simple-para></ce:abstract-sec></ce:abstract><ce:keywords class="keyword" xml:lang="en"><ce:keyword><ce:text>Indonésie</ce:text></ce:keyword><ce:keyword><ce:text>Australie</ce:text></ce:keyword><ce:keyword><ce:text>reconstructions géodynamiques</ce:text></ce:keyword><ce:keyword><ce:text>arcs volcaniques</ce:text></ce:keyword><ce:keyword><ce:text>ouverture de bassins</ce:text></ce:keyword><ce:keyword><ce:text>collisions</ce:text></ce:keyword><ce:keyword><ce:text>Éocène</ce:text></ce:keyword><ce:keyword><ce:text>Oligocène</ce:text></ce:keyword><ce:keyword><ce:text>Miocène</ce:text></ce:keyword><ce:keyword><ce:text>Pliocène</ce:text></ce:keyword></ce:keywords><ce:keywords class="keyword" xml:lang="en"><ce:keyword><ce:text>Indonesia</ce:text></ce:keyword><ce:keyword><ce:text>Australia</ce:text></ce:keyword><ce:keyword><ce:text>geodynamic reconstructions</ce:text></ce:keyword><ce:keyword><ce:text>volcanic arcs</ce:text></ce:keyword><ce:keyword><ce:text>basin openings</ce:text></ce:keyword><ce:keyword><ce:text>collisions</ce:text></ce:keyword><ce:keyword><ce:text>Eocene</ce:text></ce:keyword><ce:keyword><ce:text>Oligocene</ce:text></ce:keyword><ce:keyword><ce:text>Miocene</ce:text></ce:keyword><ce:keyword><ce:text>Pllocene</ce:text></ce:keyword></ce:keywords></head><tail><ce:bibliography><ce:section-title>Références</ce:section-title><ce:bibliography-sec><ce:bib-reference id="bib1"><ce:label>Achdan and Turkandi, 1982</ce:label><sb:reference><sb:contribution langtype="en"><sb:authors><sb:author><ce:surname>Achdan</ce:surname><ce:given-name>A.</ce:given-name></sb:author><sb:author><ce:surname>Turkandi</ce:surname><ce:given-name>T.</ce:given-name></sb:author></sb:authors><sb:title><sb:maintitle>Preliminary geological map of Kai (and Tual) Quadrangles, Maluku, Scale 1:250 000</sb:maintitle></sb:title></sb:contribution><sb:host><sb:book><sb:date>1982</sb:date><sb:publisher><sb:name>Geological Research and Developpement Centre</sb:name></sb:publisher></sb:book></sb:host></sb:reference></ce:bib-reference><ce:bib-reference id="bib2"><ce:label>Ali, et al, 1996</ce:label><sb:reference><sb:contribution langtype="en"><sb:authors><sb:author><ce:surname>Ali</ce:surname><ce:given-name>J.R.</ce:given-name></sb:author><sb:author><ce:surname>Milsom</ce:surname><ce:given-name>J.</ce:given-name></sb:author><sb:author><ce:surname>Finch</ce:surname><ce:given-name>E.M.</ce:given-name></sb:author><sb:author><ce:surname>Mubroto</ce:surname><ce:given-name>S.E.</ce:given-name></sb:author></sb:authors><sb:title><sb:maintitle>SE Sundaland accretion: palaeomagnetic evidence of large Plio-Pleistocene thin- skin rotation, <ce:italic>in</ce:italic></sb:maintitle></sb:title></sb:contribution><sb:host><sb:edited-book><sb:editors><sb:editor><ce:surname>Hall</ce:surname><ce:given-name>R.</ce:given-name></sb:editor><sb:editor><ce:surname>Blundell</ce:surname><ce:given-name>D.</ce:given-name></sb:editor></sb:editors><sb:book-series><sb:series><sb:title><sb:maintitle>Tectonic Evolution of Southeast Asia</sb:maintitle></sb:title><sb:volume-nr>106</sb:volume-nr></sb:series></sb:book-series><sb:date>1996</sb:date><sb:publisher><sb:name>Geological Society Special Publication</sb:name><sb:location>Bandung, Indonesia</sb:location></sb:publisher></sb:edited-book><sb:pages><sb:first-page>431</sb:first-page><sb:last-page>443</sb:last-page></sb:pages></sb:host></sb:reference></ce:bib-reference><ce:bib-reference id="bib3"><ce:label>Audley-Charles, et al, 1979</ce:label><sb:reference><sb:contribution langtype="en"><sb:authors><sb:author><ce:surname>Audley-Charles</ce:surname><ce:given-name>M.G.</ce:given-name></sb:author><sb:author><ce:surname>Carter</ce:surname><ce:given-name>D.J.</ce:given-name></sb:author><sb:author><ce:surname>Barber</ce:surname><ce:given-name>A.J.</ce:given-name></sb:author><sb:author><ce:surname>Norvick</ce:surname><ce:given-name>M.S.</ce:given-name></sb:author><sb:author><ce:surname>Tjokosapoetro</ce:surname><ce:given-name>S.</ce:given-name></sb:author></sb:authors><sb:title><sb:maintitle>Reinterpretation of the Geology of Seram: implications for the Banda Arc and Northern Australia</sb:maintitle></sb:title></sb:contribution><sb:host><sb:issue><sb:series><sb:title><sb:maintitle>J Geol. 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Res.</sb:maintitle></sb:title><sb:volume-nr>98</sb:volume-nr></sb:series><sb:date>1993</sb:date></sb:issue><sb:pages><sb:first-page>349</sb:first-page><sb:last-page>366</sb:last-page></sb:pages></sb:host></sb:reference></ce:bib-reference></ce:bibliography-sec></ce:bibliography></tail></article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="fr"><title>Évolution géodynamique de l'Indonésie orientale, de l'Éocène au Pliocène</title></titleInfo><titleInfo type="alternative" lang="fr" contentType="CDATA"><title>Évolution géodynamique de l'Indonésie orientale, de l'Éocène au Pliocène</title></titleInfo><titleInfo type="translated" lang="en"><title>Geodynamic evolution of Eastern Indonesia from the Eocene to the Pliocene</title></titleInfo><name type="corporate"><namePart>le groupe Géobanda</namePart></name><name type="personal"><namePart type="given">Michel</namePart><namePart type="family">Villeneuve</namePart><affiliation>Centre de sédimentologie et paléontologie, Upresa 6019, CNRS et université de Provence, case 67, 3, place Victor-Hugo, 13331 Marseille cedex 03, France</affiliation><affiliation>E-mail: mville@newsup.univ-mrs.fr</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Jean-Pierre</namePart><namePart type="family">Réhault</namePart><affiliation>Géophysique marine, UBO, BP 239, 6, av. Le-Gorgeu, 29285 Brost cedex, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Jean-Jacques</namePart><namePart type="family">Cornée</namePart><affiliation>Centre de sédimentologie et paléontologie, Upresa 6019, CNRS et université de Provence, case 67, 3, place Victor-Hugo, 13331 Marseille cedex 03, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Christian</namePart><namePart type="family">Honthaas</namePart><affiliation>Géophysique marine, UBO, BP 239, 6, av. Le-Gorgeu, 29285 Brost cedex, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Wahyu</namePart><namePart type="family">Gunawan c</namePart><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="review-article" displayLabel="Review article"></genre><originInfo><publisher>ELSEVIER</publisher><dateIssued encoding="w3cdtf">1998</dateIssued><copyrightDate encoding="w3cdtf">1998</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">fre</languageTerm><languageTerm type="code" authority="rfc3066">fr</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Abstract: Eastern Indonesia belongs to a convergent zone between the Asiatic, Australian and Pacific plates. A lot of synthetic papers have been devoted to this very technically active area. Our new geodynamic reconstruction takes into account a six year period of scientific cooperation between France and Indonesia. This cooperation provided various geological data. The hypothesis presented here is based on the geological evolution of lour small commentai blocks (two of which appear for the first time: the Banda und l.ucipara blocks) trapped by the convergence of the threemain plates. The main steps are successively: the Upper Eocene to Oligocene. during which the Banda block collided with the south east asiatic margin in Sulawesi: the Lower Miocene, during which the l.iicipara block (including (he Tukang IJesi platform) collided with the Banda block itself, mainly in the Buton area: the Upper Miocene, which is a period of large extensional regime. Most of the basins inside the Banda area opened at that time (North Banda Basin, South Banda Basin, Savu Basin, etc.). The next interesting period is the Upper Pliocene, which occurred after the main collisions between the Australian continental block and the Banda and Irian Java blocks. The Bangai Sula block collided with the eastern part of Sulawesi at the end of the Lower Pliocene.</abstract><abstract lang="fr">Résumé: L'Indonésie orientale correspond á la zone de convergence entre trois grandes plaques: Asiatique, Australienne et Pacifique. De nombreuses synthèses ont vu le jour sur cette zone particulièrement active. Nous proposons ici une nouvelle hypothèse sur Article rédigé à l'attention du Comité de lecture. Article remis le 30 mars 1998, accepté après révision le 3 août 1998. l'évolution géodynamique. Elle tient compte des nombreuses observations effectuées tant à terre qu'en mer (depuis 1989) r des équipes franco-indonésiennes. Cette hypothèse rend compte de la présence de quatre blocs de petite taille (dont deux individualisés pour la première fois: blocs de Banda et de Lucipara) qui se sont trouvés ≪ coincés ≫ entre les trois grandes plaques. Nous donnons la composition des differents blocs et leur cheminement au travers des reconstitutions paléogéographiques pour quatre périodes clés de l'évolution géologique de ette zone. Ces périodes sont: l'Éocène supérieur à l'Oligocène supérieur, au cours duquel le bloc de Banda s'est accrété à la mrge asiatique, le Miocène inférieur,au cours duquel le bloc de Lucipara est entré en collision avec le bloc de Banda, le Miocène supérieur, qui est la grande période d'extension au cours de laquelle se sont formés les principaux bassins entourés par l'arc de Banda, et le Pliocène supérieur, qui succède à la collision entre le continent australien et l'arc de Banda d'une part et lrian Jaya, d'autre part.</abstract><note type="content">Section title: Concise review paper</note><subject><genre>article-category</genre><topic>Le point sur…</topic></subject><subject lang="en"><topic>Indonésie</topic><topic>Australie</topic><topic>reconstructions géodynamiques</topic><topic>arcs volcaniques</topic><topic>ouverture de bassins</topic><topic>collisions</topic><topic>Éocène</topic><topic>Oligocène</topic><topic>Miocène</topic><topic>Pliocène</topic></subject><subject lang="en"><topic>Indonesia</topic><topic>Australia</topic><topic>geodynamic reconstructions</topic><topic>volcanic arcs</topic><topic>basin openings</topic><topic>collisions</topic><topic>Eocene</topic><topic>Oligocene</topic><topic>Miocene</topic><topic>Pllocene</topic></subject><relatedItem type="host"><titleInfo><title>Comptes Rendus de l'Academie des Sciences Series IIA Earth and Planetary Science</title></titleInfo><titleInfo type="abbreviated"><title>PXTOLD</title></titleInfo><genre type="journal">journal</genre><originInfo><dateIssued encoding="w3cdtf">199809</dateIssued></originInfo><identifier type="ISSN">1251-8050</identifier><identifier type="PII">S1251-8050(00)X0092-4</identifier><part><date>199809</date><detail type="volume"><number>327</number><caption>vol.</caption></detail><detail type="issue"><number>5</number><caption>no.</caption></detail><extent unit="issue pages"><start>291</start><end>360</end></extent><extent unit="pages"><start>291</start><end>302</end></extent></part></relatedItem><identifier type="istex">79143E3277C8F236120CC1CEC0B1B207B43043E8</identifier><identifier type="DOI">10.1016/S1251-8050(98)80046-3</identifier><identifier type="PII">S1251-8050(98)80046-3</identifier><identifier type="ArticleID">98800463</identifier><accessCondition type="use and reproduction" contentType="copyright">©1998 Académie des sciences/Elsevier, Paris</accessCondition><recordInfo><recordContentSource>ELSEVIER</recordContentSource><recordOrigin>Académie des sciences/Elsevier, Paris, ©1998</recordOrigin></recordInfo></mods></metadata></istex></record>Pour manipuler ce document sous Unix (Dilib)
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