Source to sink relations between the Tian Shan and Junggar Basin (northwest China) from Late Palaeozoic to Quaternary: evidence from detrital U‐Pb zircon geochronology
Identifieur interne : 001E79 ( Istex/Corpus ); précédent : 001E78; suivant : 001E80Source to sink relations between the Tian Shan and Junggar Basin (northwest China) from Late Palaeozoic to Quaternary: evidence from detrital U‐Pb zircon geochronology
Auteurs : Wei Yang ; Marc Jolivet ; Guillaume Dupont-Nivet ; Zhaojie Guo ; Zhicheng Zhang ; Chaodong WuSource :
- Basin Research [ 0950-091X ] ; 2013-04.
Abstract
The tectonic evolution of the Tian Shan, as for most ranges in continental Asia is dominated by north‐south compression since the Cenozoic India‐Asia collision. However, precollision governing tectonic processes remain enigmatic. An excellent record is provided by thick Palaeozoic – Cenozoic lacustrine to fluvial depositional sequences that are well preserved in the southern margin of the Junggar Basin and exposed along a foreland basin associated to the Late Cenozoic rejuvenation of the Tian Shan ranges. U/Pb (LA‐ICP‐MS) dating of detrital zircons from 14 sandstone samples from a continuous series ranging in age from latest Palaeozoic to Quaternary is used to investigate changes in sediment provenance through time and to correlate them with major tectonic phases in the range. Samples were systematically collected along two nearby sections in the foreland basin. The results show that the detrital zircons are mostly magmatic in origin, with some minor input from metamorphic zircons. The U‐Pb detrital zircon ages range widely from 127 to 2856 Ma and can be divided into four main groups: 127–197 (sub‐peak at 159 Ma), 250–379 (sub‐peak at 318 Ma), 381–538 (sub‐peak at 406 Ma) and 543–2856 Ma (sub‐peak at 912 Ma). These groups indicate that the zircons were largely derived from the Tian Shan area to the south since a Late Carboniferous basin initiation. The provenance and basin‐range pattern evolution of the southern margin of Junggar Basin can be generally divided into four stages: (1) Late Carboniferous – Early Triassic basin evolution in a half‐graben or post‐orogenic extensional context; (2) From Middle Triassic to Upper Jurassic times, the southern Junggar became a passively subsiding basin until (3) being inverted during Lower Cretaceous – Palaeogene; (4) During the Neogene, a piedmont developed along the northern margin of the North Tian Shan block and Junggar Basin became a true foreland basin.
Url:
DOI: 10.1111/j.1365-2117.2012.00558.x
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<front><div type="abstract">The tectonic evolution of the Tian Shan, as for most ranges in continental Asia is dominated by north‐south compression since the Cenozoic India‐Asia collision. However, precollision governing tectonic processes remain enigmatic. An excellent record is provided by thick Palaeozoic – Cenozoic lacustrine to fluvial depositional sequences that are well preserved in the southern margin of the Junggar Basin and exposed along a foreland basin associated to the Late Cenozoic rejuvenation of the Tian Shan ranges. U/Pb (LA‐ICP‐MS) dating of detrital zircons from 14 sandstone samples from a continuous series ranging in age from latest Palaeozoic to Quaternary is used to investigate changes in sediment provenance through time and to correlate them with major tectonic phases in the range. Samples were systematically collected along two nearby sections in the foreland basin. The results show that the detrital zircons are mostly magmatic in origin, with some minor input from metamorphic zircons. The U‐Pb detrital zircon ages range widely from 127 to 2856 Ma and can be divided into four main groups: 127–197 (sub‐peak at 159 Ma), 250–379 (sub‐peak at 318 Ma), 381–538 (sub‐peak at 406 Ma) and 543–2856 Ma (sub‐peak at 912 Ma). These groups indicate that the zircons were largely derived from the Tian Shan area to the south since a Late Carboniferous basin initiation. The provenance and basin‐range pattern evolution of the southern margin of Junggar Basin can be generally divided into four stages: (1) Late Carboniferous – Early Triassic basin evolution in a half‐graben or post‐orogenic extensional context; (2) From Middle Triassic to Upper Jurassic times, the southern Junggar became a passively subsiding basin until (3) being inverted during Lower Cretaceous – Palaeogene; (4) During the Neogene, a piedmont developed along the northern margin of the North Tian Shan block and Junggar Basin became a true foreland basin.</div>
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<abstract>The tectonic evolution of the Tian Shan, as for most ranges in continental Asia is dominated by north‐south compression since the Cenozoic India‐Asia collision. However, precollision governing tectonic processes remain enigmatic. An excellent record is provided by thick Palaeozoic – Cenozoic lacustrine to fluvial depositional sequences that are well preserved in the southern margin of the Junggar Basin and exposed along a foreland basin associated to the Late Cenozoic rejuvenation of the Tian Shan ranges. U/Pb (LA‐ICP‐MS) dating of detrital zircons from 14 sandstone samples from a continuous series ranging in age from latest Palaeozoic to Quaternary is used to investigate changes in sediment provenance through time and to correlate them with major tectonic phases in the range. Samples were systematically collected along two nearby sections in the foreland basin. The results show that the detrital zircons are mostly magmatic in origin, with some minor input from metamorphic zircons. The U‐Pb detrital zircon ages range widely from 127 to 2856 Ma and can be divided into four main groups: 127–197 (sub‐peak at 159 Ma), 250–379 (sub‐peak at 318 Ma), 381–538 (sub‐peak at 406 Ma) and 543–2856 Ma (sub‐peak at 912 Ma). These groups indicate that the zircons were largely derived from the Tian Shan area to the south since a Late Carboniferous basin initiation. The provenance and basin‐range pattern evolution of the southern margin of Junggar Basin can be generally divided into four stages: (1) Late Carboniferous – Early Triassic basin evolution in a half‐graben or post‐orogenic extensional context; (2) From Middle Triassic to Upper Jurassic times, the southern Junggar became a passively subsiding basin until (3) being inverted during Lower Cretaceous – Palaeogene; (4) During the Neogene, a piedmont developed along the northern margin of the North Tian Shan block and Junggar Basin became a true foreland basin.</abstract>
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<notesStmt><note>Appendix S1: U‐Pb Geochronologic Analysis of Detrital Zircons from the 14 Sandstone Samples.Appendix S2: Representative CL Images of Zircons from the 14 Sandstone Samples. White Circles Show the Location of U‐Pb Analysis. Numbers are U‐Pb Ages in Ma. </note>
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<note>Egide Cai Yuanpei program</note>
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<sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Source to sink relations between the Tian Shan and Junggar Basin (northwest China) from Late Palaeozoic to Quaternary: evidence from detrital U‐Pb zircon geochronology</title>
<author xml:id="author-1"><persName><forename type="first">Wei</forename>
<surname>Yang</surname>
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<affiliation>Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing, China</affiliation>
</author>
<author xml:id="author-2"><persName><forename type="first">Marc</forename>
<surname>Jolivet</surname>
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<affiliation>Géosciences Rennes, Université Rennes 1, Rennes, France</affiliation>
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<author xml:id="author-3"><persName><forename type="first">Guillaume</forename>
<surname>Dupont‐Nivet</surname>
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<affiliation>Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing, China</affiliation>
<affiliation>Géosciences Rennes, Université Rennes 1, Rennes, France</affiliation>
<affiliation>Faculty of Geosciences, Utrecht University, Utrecht, The Netherlands</affiliation>
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<author xml:id="author-4"><persName><forename type="first">Zhaojie</forename>
<surname>Guo</surname>
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<email>zjguo@pku.edu.cn</email>
<affiliation>Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing, China</affiliation>
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<author xml:id="author-5"><persName><forename type="first">Zhicheng</forename>
<surname>Zhang</surname>
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<affiliation>Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing, China</affiliation>
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<abstract><p>The tectonic evolution of the Tian Shan, as for most ranges in continental Asia is dominated by north‐south compression since the Cenozoic India‐Asia collision. However, precollision governing tectonic processes remain enigmatic. An excellent record is provided by thick Palaeozoic – Cenozoic lacustrine to fluvial depositional sequences that are well preserved in the southern margin of the Junggar Basin and exposed along a foreland basin associated to the Late Cenozoic rejuvenation of the Tian Shan ranges. U/Pb (LA‐ICP‐MS) dating of detrital zircons from 14 sandstone samples from a continuous series ranging in age from latest Palaeozoic to Quaternary is used to investigate changes in sediment provenance through time and to correlate them with major tectonic phases in the range. Samples were systematically collected along two nearby sections in the foreland basin. The results show that the detrital zircons are mostly magmatic in origin, with some minor input from metamorphic zircons. The U‐Pb detrital zircon ages range widely from 127 to 2856 Ma and can be divided into four main groups: 127–197 (sub‐peak at 159 Ma), 250–379 (sub‐peak at 318 Ma), 381–538 (sub‐peak at 406 Ma) and 543–2856 Ma (sub‐peak at 912 Ma). These groups indicate that the zircons were largely derived from the Tian Shan area to the south since a Late Carboniferous basin initiation. The provenance and basin‐range pattern evolution of the southern margin of Junggar Basin can be generally divided into four stages: (1) Late Carboniferous – Early Triassic basin evolution in a half‐graben or post‐orogenic extensional context; (2) From Middle Triassic to Upper Jurassic times, the southern Junggar became a passively subsiding basin until (3) being inverted during Lower Cretaceous – Palaeogene; (4) During the Neogene, a piedmont developed along the northern margin of the North Tian Shan block and Junggar Basin became a true foreland basin.</p>
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<titleGroup><title sort="BASIN RESEARCH" type="main">Basin Research</title>
<title type="short">Basin Res</title>
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<publicationMeta level="part" position="20"><doi origin="wiley">10.1111/bre.2013.25.issue-2</doi>
<copyright ownership="publisher">Basin Research © 2013 Blackwell Publishing Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologists</copyright>
<numberingGroup><numbering type="journalVolume" number="25">25</numbering>
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<coverDate startDate="2013-04">April 2013</coverDate>
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<publicationMeta level="unit" position="50" status="forIssue" type="article"><doi>10.1111/j.1365-2117.2012.00558.x</doi>
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<titleGroup><title type="articleCategory">Original Article</title>
<title type="tocHeading1">Original Articles</title>
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<copyright ownership="joint">© 2012 The Authors. Basin Research © 2012 Blackwell Publishing Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologists</copyright>
<eventGroup><event date="2011-06-25" type="manuscriptReceived"></event>
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<correspondenceTo>Correspondence: Z. Guo, Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing, China 100871. E‐mail: <email>zjguo@pku.edu.cn</email>
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<contentMeta><titleGroup><title type="main">Source to sink relations between the Tian Shan and Junggar Basin (northwest China) from Late Palaeozoic to Quaternary: evidence from detrital U‐Pb zircon geochronology</title>
<title type="shortAuthors"><i>W. Yang</i>
et al.</title>
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<creators><creator affiliationRef="#bre558-aff-0001" creatorRole="author" xml:id="bre558-cr-0001"><personName><givenNames>Wei</givenNames>
<familyName>Yang</familyName>
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<creator affiliationRef="#bre558-aff-0002" creatorRole="author" xml:id="bre558-cr-0002"><personName><givenNames>Marc</givenNames>
<familyName>Jolivet</familyName>
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<creator affiliationRef="#bre558-aff-0001 #bre558-aff-0002 #bre558-aff-0003" creatorRole="author" xml:id="bre558-cr-0003"><personName><givenNames>Guillaume</givenNames>
<familyName>Dupont‐Nivet</familyName>
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<creator affiliationRef="#bre558-aff-0001" corresponding="yes" creatorRole="author" xml:id="bre558-cr-0004"><personName><givenNames>Zhaojie</givenNames>
<familyName>Guo</familyName>
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<creator affiliationRef="#bre558-aff-0001" creatorRole="author" xml:id="bre558-cr-0005"><personName><givenNames>Zhicheng</givenNames>
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<creator affiliationRef="#bre558-aff-0001" creatorRole="author" xml:id="bre558-cr-0006"><personName><givenNames>Chaodong</givenNames>
<familyName>Wu</familyName>
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<affiliationGroup><affiliation countryCode="CN" type="organization" xml:id="bre558-aff-0001"><orgDiv>Key Laboratory of Orogenic Belts and Crustal Evolution</orgDiv>
<orgDiv>Ministry of Education</orgDiv>
<orgDiv>School of Earth and Space Sciences</orgDiv>
<orgName>Peking University</orgName>
<address><city>Beijing</city>
<country>China</country>
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<affiliation countryCode="FR" type="organization" xml:id="bre558-aff-0002"><orgDiv>Géosciences Rennes</orgDiv>
<orgName>Université Rennes 1</orgName>
<address><city>Rennes</city>
<country>France</country>
</address>
</affiliation>
<affiliation countryCode="NL" type="organization" xml:id="bre558-aff-0003"><orgDiv>Faculty of Geosciences</orgDiv>
<orgName>Utrecht University</orgName>
<address><city>Utrecht</city>
<country>The Netherlands</country>
</address>
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<fundingInfo><fundingAgency>State Science and Technology</fundingAgency>
<fundingNumber>2011ZX05009‐001</fundingNumber>
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<fundingInfo><fundingAgency>Egide Cai Yuanpei program</fundingAgency>
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<caption><b>Appendix S1:</b>
U‐Pb Geochronologic Analysis of Detrital Zircons from the 14 Sandstone Samples.</caption>
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<caption><b>Appendix S2:</b>
Representative CL Images of Zircons from the 14 Sandstone Samples. White Circles Show the Location of U‐Pb Analysis. Numbers are U‐Pb Ages in Ma.</caption>
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<abstractGroup><abstract type="main" xml:id="bre558-abs-0001"><title type="main">Abstract</title>
<p>The tectonic evolution of the Tian Shan, as for most ranges in continental Asia is dominated by north‐south compression since the Cenozoic India‐Asia collision. However, precollision governing tectonic processes remain enigmatic. An excellent record is provided by thick Palaeozoic – Cenozoic lacustrine to fluvial depositional sequences that are well preserved in the southern margin of the Junggar Basin and exposed along a foreland basin associated to the Late Cenozoic rejuvenation of the Tian Shan ranges. U/Pb (<fc>LA</fc>
‐<fc>ICP</fc>
‐<fc>MS</fc>
) dating of detrital zircons from 14 sandstone samples from a continuous series ranging in age from latest Palaeozoic to Quaternary is used to investigate changes in sediment provenance through time and to correlate them with major tectonic phases in the range. Samples were systematically collected along two nearby sections in the foreland basin. The results show that the detrital zircons are mostly magmatic in origin, with some minor input from metamorphic zircons. The U‐Pb detrital zircon ages range widely from 127 to 2856 Ma and can be divided into four main groups: 127–197 (sub‐peak at 159 Ma), 250–379 (sub‐peak at 318 Ma), 381–538 (sub‐peak at 406 Ma) and 543–2856 Ma (sub‐peak at 912 Ma). These groups indicate that the zircons were largely derived from the Tian Shan area to the south since a Late Carboniferous basin initiation. The provenance and basin‐range pattern evolution of the southern margin of Junggar Basin can be generally divided into four stages: (1) Late Carboniferous – Early Triassic basin evolution in a half‐graben or post‐orogenic extensional context; (2) From Middle Triassic to Upper Jurassic times, the southern Junggar became a passively subsiding basin until (3) being inverted during Lower Cretaceous – Palaeogene; (4) During the Neogene, a piedmont developed along the northern margin of the North Tian Shan block and Junggar Basin became a true foreland basin.</p>
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<name type="personal"><namePart type="given">Wei</namePart>
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<name type="personal"><namePart type="given">Marc</namePart>
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<name type="personal"><namePart type="given">Guillaume</namePart>
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<affiliation>Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing, China</affiliation>
<affiliation>Géosciences Rennes, Université Rennes 1, Rennes, France</affiliation>
<affiliation>Faculty of Geosciences, Utrecht University, Utrecht, The Netherlands</affiliation>
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<name type="personal"><namePart type="given">Zhicheng</namePart>
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<name type="personal"><namePart type="given">Chaodong</namePart>
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<abstract>The tectonic evolution of the Tian Shan, as for most ranges in continental Asia is dominated by north‐south compression since the Cenozoic India‐Asia collision. However, precollision governing tectonic processes remain enigmatic. An excellent record is provided by thick Palaeozoic – Cenozoic lacustrine to fluvial depositional sequences that are well preserved in the southern margin of the Junggar Basin and exposed along a foreland basin associated to the Late Cenozoic rejuvenation of the Tian Shan ranges. U/Pb (LA‐ICP‐MS) dating of detrital zircons from 14 sandstone samples from a continuous series ranging in age from latest Palaeozoic to Quaternary is used to investigate changes in sediment provenance through time and to correlate them with major tectonic phases in the range. Samples were systematically collected along two nearby sections in the foreland basin. The results show that the detrital zircons are mostly magmatic in origin, with some minor input from metamorphic zircons. The U‐Pb detrital zircon ages range widely from 127 to 2856 Ma and can be divided into four main groups: 127–197 (sub‐peak at 159 Ma), 250–379 (sub‐peak at 318 Ma), 381–538 (sub‐peak at 406 Ma) and 543–2856 Ma (sub‐peak at 912 Ma). These groups indicate that the zircons were largely derived from the Tian Shan area to the south since a Late Carboniferous basin initiation. The provenance and basin‐range pattern evolution of the southern margin of Junggar Basin can be generally divided into four stages: (1) Late Carboniferous – Early Triassic basin evolution in a half‐graben or post‐orogenic extensional context; (2) From Middle Triassic to Upper Jurassic times, the southern Junggar became a passively subsiding basin until (3) being inverted during Lower Cretaceous – Palaeogene; (4) During the Neogene, a piedmont developed along the northern margin of the North Tian Shan block and Junggar Basin became a true foreland basin.</abstract>
<note type="additional physical form">Appendix S1: U‐Pb Geochronologic Analysis of Detrital Zircons from the 14 Sandstone Samples.Appendix S2: Representative CL Images of Zircons from the 14 Sandstone Samples. White Circles Show the Location of U‐Pb Analysis. Numbers are U‐Pb Ages in Ma. </note>
<note type="funding">State Science and Technology - No. 2011ZX05009‐001; </note>
<note type="funding">Egide Cai Yuanpei program</note>
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