Erratiques de dolomie au cap Colombier, sur la haute côte-nord du Saint-Laurent estuarien
Identifieur interne : 000287 ( PascalFrancis/Corpus ); précédent : 000286; suivant : 000288Erratiques de dolomie au cap Colombier, sur la haute côte-nord du Saint-Laurent estuarien
Auteurs : Jean-Claude DionneSource :
- Géogr. Phys. Quat. [ 0705-7199 ] ; 2001.
Descripteurs français
- Pascal (Inist)
- Age absolu, C 14, Cénozoïque, Milieu littoral, Dolomie, Canada Est, Bloc erratique, Coulée, Transport glaciaire, Holocène, Isotope, Holocène inf, Paléoclimatologie, Québec, Isotope radioactif, Estuaire Saint Laurent, Striation, Géochronologie, Stratigraphie, Sédimentation, Pétrologie roche sédimentaire, Milieu, Glaciologie, Géomorphologie, Géochimie, Structure sédimentaire, Irrégularité plan stratification.
English descriptors
- KwdEn :
- C-14, Cape Colombier, Cenozoic, Eastern Canada, Holocene, Quebec, Saint Lawrence Estuary, absolute age, bedding plane irregularities, coastal environment, dolostone, environment, erratics, flows, geochemistry, geochronology, geomorphology, glacial transport, glaciology, isotopes, lower Holocene, paleoclimatology, radioactive isotopes, sedimentary petrology, sedimentary structures, sedimentation, stratigraphy, striations.
Abstract
At about 150 km NE of Tadoussac, Cap Colombier is presently the most northeastern site known along the north shore of the lower St. Lawrence estuary where dolostone erratics occur in a significant amount. Over 50 dolostone erratics of various types have been observed in the intertidal clayey zone of Havre du Colombier. The size of clasts ranges from 7 to 320 cm. Although one mega-boulder weighs about 20 metric tons, the remaining erratics are much smaller, the ten largest weighing between 33 and 345 kg. About 12% of the clasts were crystalline pink dolostone and 20% were striated. One brecchiated boulder contained stromatolitic structures. The most likely source is the Mistassini sedimentary basin located about 500 km to the NW. This suggests first a glacial transport by a major ice flow from an ice divide located NW of Lake Mistassini, and second, a release in the Goldthwait Sea by icebergs possibly calved from the glacier tongue located in the Saguenay fjord.
Notice en format standard (ISO 2709)
Pour connaître la documentation sur le format Inist Standard.
pA |
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Format Inist (serveur)
NO : | PASCAL 03-0360252 AGI |
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FT : | Erratiques de dolomie au cap Colombier, sur la haute côte-nord du Saint-Laurent estuarien |
ET : | (Dolostone erratics at Cape Colombier, upper north coast of the Saint Lawrence Estuary) |
AU : | DIONNE (Jean-Claude) |
AF : | Université Laval, Département de Géographie/Sainte-Foy, PQ/Canada |
DT : | Publication en série; Niveau analytique |
SO : | Géogr. Phys. Quat.; ISSN 0705-7199; Canada; Da. 2001; Vol. 55; No. 1; Pp. 101-107; Abs. anglais; Bibl. 22 ref. |
LA : | Français |
EA : | At about 150 km NE of Tadoussac, Cap Colombier is presently the most northeastern site known along the north shore of the lower St. Lawrence estuary where dolostone erratics occur in a significant amount. Over 50 dolostone erratics of various types have been observed in the intertidal clayey zone of Havre du Colombier. The size of clasts ranges from 7 to 320 cm. Although one mega-boulder weighs about 20 metric tons, the remaining erratics are much smaller, the ten largest weighing between 33 and 345 kg. About 12% of the clasts were crystalline pink dolostone and 20% were striated. One brecchiated boulder contained stromatolitic structures. The most likely source is the Mistassini sedimentary basin located about 500 km to the NW. This suggests first a glacial transport by a major ice flow from an ice divide located NW of Lake Mistassini, and second, a release in the Goldthwait Sea by icebergs possibly calved from the glacier tongue located in the Saguenay fjord. |
CC : | 226C02; 223A01; 001E01P02; 001E01G01 |
FD : | Age absolu; C 14; Cénozoïque; Milieu littoral; Dolomie; Canada Est; Bloc erratique; Coulée; Transport glaciaire; Holocène; Isotope; Holocène inf; Paléoclimatologie; Québec; Isotope radioactif; Estuaire Saint Laurent; Striation; Géochronologie; Stratigraphie; Sédimentation; Pétrologie roche sédimentaire; Milieu; Glaciologie; Géomorphologie; Géochimie; Structure sédimentaire; Irrégularité plan stratification |
FG : | Phanérozoïque; Roche carbonatée; Roche sédimentaire; Canada; Amérique du Nord; Quaternaire sup; Quaternaire |
ED : | absolute age; C-14; Cenozoic; coastal environment; dolostone; Eastern Canada; erratics; flows; glacial transport; Holocene; isotopes; lower Holocene; paleoclimatology; Quebec; radioactive isotopes; Saint Lawrence Estuary; striations; geochronology; stratigraphy; sedimentation; sedimentary petrology; environment; glaciology; geomorphology; geochemistry; sedimentary structures; Cape Colombier; bedding plane irregularities |
EG : | Phanerozoic; carbonate rocks; sedimentary rocks; Canada; North America; upper Quaternary; Quaternary |
SD : | C 14; Cenozoico; Medio litoral; Dolomía; Canadá Este; Bloque errático; Colada; Transporte glaciar; Holoceno; Isótopo; Holoceno inf; Quebec; Isótopo radioactivo; Estuario San Lorenzo; Estriación; Geocronología; Estratigrafía; Sedimentación; Petrología roca sedimentaria; Medio; Geomorfología; Geoquímica; Estructura sedimentaria |
LO : | AGI |
ID : | 03-0360252 |
Links to Exploration step
Pascal:03-0360252Le document en format XML
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<sourceDesc><biblStruct><analytic><title xml:lang="fr" level="a">Erratiques de dolomie au cap Colombier, sur la haute côte-nord du Saint-Laurent estuarien</title>
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>C-14</term>
<term>Cape Colombier</term>
<term>Cenozoic</term>
<term>Eastern Canada</term>
<term>Holocene</term>
<term>Quebec</term>
<term>Saint Lawrence Estuary</term>
<term>absolute age</term>
<term>bedding plane irregularities</term>
<term>coastal environment</term>
<term>dolostone</term>
<term>environment</term>
<term>erratics</term>
<term>flows</term>
<term>geochemistry</term>
<term>geochronology</term>
<term>geomorphology</term>
<term>glacial transport</term>
<term>glaciology</term>
<term>isotopes</term>
<term>lower Holocene</term>
<term>paleoclimatology</term>
<term>radioactive isotopes</term>
<term>sedimentary petrology</term>
<term>sedimentary structures</term>
<term>sedimentation</term>
<term>stratigraphy</term>
<term>striations</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Age absolu</term>
<term>C 14</term>
<term>Cénozoïque</term>
<term>Milieu littoral</term>
<term>Dolomie</term>
<term>Canada Est</term>
<term>Bloc erratique</term>
<term>Coulée</term>
<term>Transport glaciaire</term>
<term>Holocène</term>
<term>Isotope</term>
<term>Holocène inf</term>
<term>Paléoclimatologie</term>
<term>Québec</term>
<term>Isotope radioactif</term>
<term>Estuaire Saint Laurent</term>
<term>Striation</term>
<term>Géochronologie</term>
<term>Stratigraphie</term>
<term>Sédimentation</term>
<term>Pétrologie roche sédimentaire</term>
<term>Milieu</term>
<term>Glaciologie</term>
<term>Géomorphologie</term>
<term>Géochimie</term>
<term>Structure sédimentaire</term>
<term>Irrégularité plan stratification</term>
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<front><div type="abstract" xml:lang="en">At about 150 km NE of Tadoussac, Cap Colombier is presently the most northeastern site known along the north shore of the lower St. Lawrence estuary where dolostone erratics occur in a significant amount. Over 50 dolostone erratics of various types have been observed in the intertidal clayey zone of Havre du Colombier. The size of clasts ranges from 7 to 320 cm. Although one mega-boulder weighs about 20 metric tons, the remaining erratics are much smaller, the ten largest weighing between 33 and 345 kg. About 12% of the clasts were crystalline pink dolostone and 20% were striated. One brecchiated boulder contained stromatolitic structures. The most likely source is the Mistassini sedimentary basin located about 500 km to the NW. This suggests first a glacial transport by a major ice flow from an ice divide located NW of Lake Mistassini, and second, a release in the Goldthwait Sea by icebergs possibly calved from the glacier tongue located in the Saguenay fjord.</div>
</front>
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<fA03 i2="1"><s0>Géogr. Phys. Quat.</s0>
</fA03>
<fA05><s2>55</s2>
</fA05>
<fA06><s2>1</s2>
</fA06>
<fA08 i1="01" i2="1" l="FRE"><s1>Erratiques de dolomie au cap Colombier, sur la haute côte-nord du Saint-Laurent estuarien</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>DIONNE (Jean-Claude)</s1>
</fA11>
<fA14 i1="01"><s1>Université Laval, Département de Géographie</s1>
<s2>Sainte-Foy, PQ</s2>
<s3>CAN</s3>
</fA14>
<fA20><s1>101-107</s1>
<s7>4</s7>
</fA20>
<fA21><s1>2001</s1>
</fA21>
<fA23 i1="01"><s0>FRE</s0>
</fA23>
<fA24 i1="01"><s0>eng</s0>
</fA24>
<fA43 i1="01"><s1>AGI</s1>
</fA43>
<fA44><s0>6000</s0>
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<fA60><s1>P</s1>
</fA60>
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<fA66 i1="01"><s0>CAN</s0>
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<fA68 i1="01" i2="1" l="ENG"><s1>Dolostone erratics at Cape Colombier, upper north coast of the Saint Lawrence Estuary</s1>
</fA68>
<fC01 i1="01" l="ENG"><s0>At about 150 km NE of Tadoussac, Cap Colombier is presently the most northeastern site known along the north shore of the lower St. Lawrence estuary where dolostone erratics occur in a significant amount. Over 50 dolostone erratics of various types have been observed in the intertidal clayey zone of Havre du Colombier. The size of clasts ranges from 7 to 320 cm. Although one mega-boulder weighs about 20 metric tons, the remaining erratics are much smaller, the ten largest weighing between 33 and 345 kg. About 12% of the clasts were crystalline pink dolostone and 20% were striated. One brecchiated boulder contained stromatolitic structures. The most likely source is the Mistassini sedimentary basin located about 500 km to the NW. This suggests first a glacial transport by a major ice flow from an ice divide located NW of Lake Mistassini, and second, a release in the Goldthwait Sea by icebergs possibly calved from the glacier tongue located in the Saguenay fjord.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>226C02</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>223A01</s0>
</fC02>
<fC02 i1="03" i2="X"><s0>001E01P02</s0>
</fC02>
<fC02 i1="04" i2="X"><s0>001E01G01</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Age absolu</s0>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>absolute age</s0>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>C 14</s0>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>C-14</s0>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>C 14</s0>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Cénozoïque</s0>
<s2>NX</s2>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>Cenozoic</s0>
<s2>NX</s2>
</fC03>
<fC03 i1="03" i2="2" l="SPA"><s0>Cenozoico</s0>
<s2>NX</s2>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Milieu littoral</s0>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>coastal environment</s0>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Medio litoral</s0>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Dolomie</s0>
<s2>NV</s2>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>dolostone</s0>
<s2>NV</s2>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Dolomía</s0>
<s2>NV</s2>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Canada Est</s0>
<s2>NG</s2>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>Eastern Canada</s0>
<s2>NG</s2>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Canadá Este</s0>
<s2>NG</s2>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Bloc erratique</s0>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>erratics</s0>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Bloque errático</s0>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Coulée</s0>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>flows</s0>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Colada</s0>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Transport glaciaire</s0>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>glacial transport</s0>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Transporte glaciar</s0>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Holocène</s0>
<s2>NX</s2>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>Holocene</s0>
<s2>NX</s2>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Holoceno</s0>
<s2>NX</s2>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Isotope</s0>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>isotopes</s0>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Isótopo</s0>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Holocène inf</s0>
<s2>NX</s2>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>lower Holocene</s0>
<s2>NX</s2>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Holoceno inf</s0>
<s2>NX</s2>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Paléoclimatologie</s0>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>paleoclimatology</s0>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Québec</s0>
<s2>NG</s2>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>Quebec</s0>
<s2>NG</s2>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Quebec</s0>
<s2>NG</s2>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Isotope radioactif</s0>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>radioactive isotopes</s0>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Isótopo radioactivo</s0>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Estuaire Saint Laurent</s0>
<s2>NG</s2>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>Saint Lawrence Estuary</s0>
<s2>NG</s2>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Estuario San Lorenzo</s0>
<s2>NG</s2>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Striation</s0>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>striations</s0>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Estriación</s0>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Géochronologie</s0>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>geochronology</s0>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Geocronología</s0>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Stratigraphie</s0>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>stratigraphy</s0>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Estratigrafía</s0>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Sédimentation</s0>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>sedimentation</s0>
</fC03>
<fC03 i1="20" i2="2" l="SPA"><s0>Sedimentación</s0>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Pétrologie roche sédimentaire</s0>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>sedimentary petrology</s0>
</fC03>
<fC03 i1="21" i2="2" l="SPA"><s0>Petrología roca sedimentaria</s0>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Milieu</s0>
</fC03>
<fC03 i1="22" i2="2" l="ENG"><s0>environment</s0>
</fC03>
<fC03 i1="22" i2="2" l="SPA"><s0>Medio</s0>
</fC03>
<fC03 i1="23" i2="2" l="FRE"><s0>Glaciologie</s0>
</fC03>
<fC03 i1="23" i2="2" l="ENG"><s0>glaciology</s0>
</fC03>
<fC03 i1="24" i2="2" l="FRE"><s0>Géomorphologie</s0>
</fC03>
<fC03 i1="24" i2="2" l="ENG"><s0>geomorphology</s0>
</fC03>
<fC03 i1="24" i2="2" l="SPA"><s0>Geomorfología</s0>
</fC03>
<fC03 i1="25" i2="2" l="FRE"><s0>Géochimie</s0>
</fC03>
<fC03 i1="25" i2="2" l="ENG"><s0>geochemistry</s0>
</fC03>
<fC03 i1="25" i2="2" l="SPA"><s0>Geoquímica</s0>
</fC03>
<fC03 i1="26" i2="2" l="FRE"><s0>Structure sédimentaire</s0>
</fC03>
<fC03 i1="26" i2="2" l="ENG"><s0>sedimentary structures</s0>
</fC03>
<fC03 i1="26" i2="2" l="SPA"><s0>Estructura sedimentaria</s0>
</fC03>
<fC03 i1="27" i2="2" l="ENG"><s0>Cape Colombier</s0>
<s4>INC</s4>
</fC03>
<fC03 i1="28" i2="2" l="FRE"><s0>Irrégularité plan stratification</s0>
</fC03>
<fC03 i1="28" i2="2" l="ENG"><s0>bedding plane irregularities</s0>
</fC03>
<fC06><s0>TAS</s0>
<s0>SKS</s0>
</fC06>
<fC07 i1="01" i2="2" l="FRE"><s0>Phanérozoïque</s0>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Phanerozoic</s0>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Fanerozoico</s0>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Roche carbonatée</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>carbonate rocks</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Roca carbonatada</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Roche sédimentaire</s0>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>sedimentary rocks</s0>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Roca sedimentaria</s0>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Canada</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Canada</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Canada</s0>
<s2>NG</s2>
</fC07>
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<fC07 i1="06" i2="2" l="FRE"><s0>Quaternaire sup</s0>
<s2>NX</s2>
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<fC07 i1="06" i2="2" l="ENG"><s0>upper Quaternary</s0>
<s2>NX</s2>
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<fC07 i1="06" i2="2" l="SPA"><s0>Cuaternario sup</s0>
<s2>NX</s2>
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<fC07 i1="07" i2="2" l="FRE"><s0>Quaternaire</s0>
<s2>NX</s2>
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<fC07 i1="07" i2="2" l="ENG"><s0>Quaternary</s0>
<s2>NX</s2>
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<server><NO>PASCAL 03-0360252 AGI</NO>
<FT>Erratiques de dolomie au cap Colombier, sur la haute côte-nord du Saint-Laurent estuarien</FT>
<ET>(Dolostone erratics at Cape Colombier, upper north coast of the Saint Lawrence Estuary)</ET>
<AU>DIONNE (Jean-Claude)</AU>
<AF>Université Laval, Département de Géographie/Sainte-Foy, PQ/Canada</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Géogr. Phys. Quat.; ISSN 0705-7199; Canada; Da. 2001; Vol. 55; No. 1; Pp. 101-107; Abs. anglais; Bibl. 22 ref.</SO>
<LA>Français</LA>
<EA>At about 150 km NE of Tadoussac, Cap Colombier is presently the most northeastern site known along the north shore of the lower St. Lawrence estuary where dolostone erratics occur in a significant amount. Over 50 dolostone erratics of various types have been observed in the intertidal clayey zone of Havre du Colombier. The size of clasts ranges from 7 to 320 cm. Although one mega-boulder weighs about 20 metric tons, the remaining erratics are much smaller, the ten largest weighing between 33 and 345 kg. About 12% of the clasts were crystalline pink dolostone and 20% were striated. One brecchiated boulder contained stromatolitic structures. The most likely source is the Mistassini sedimentary basin located about 500 km to the NW. This suggests first a glacial transport by a major ice flow from an ice divide located NW of Lake Mistassini, and second, a release in the Goldthwait Sea by icebergs possibly calved from the glacier tongue located in the Saguenay fjord.</EA>
<CC>226C02; 223A01; 001E01P02; 001E01G01</CC>
<FD>Age absolu; C 14; Cénozoïque; Milieu littoral; Dolomie; Canada Est; Bloc erratique; Coulée; Transport glaciaire; Holocène; Isotope; Holocène inf; Paléoclimatologie; Québec; Isotope radioactif; Estuaire Saint Laurent; Striation; Géochronologie; Stratigraphie; Sédimentation; Pétrologie roche sédimentaire; Milieu; Glaciologie; Géomorphologie; Géochimie; Structure sédimentaire; Irrégularité plan stratification</FD>
<FG>Phanérozoïque; Roche carbonatée; Roche sédimentaire; Canada; Amérique du Nord; Quaternaire sup; Quaternaire</FG>
<ED>absolute age; C-14; Cenozoic; coastal environment; dolostone; Eastern Canada; erratics; flows; glacial transport; Holocene; isotopes; lower Holocene; paleoclimatology; Quebec; radioactive isotopes; Saint Lawrence Estuary; striations; geochronology; stratigraphy; sedimentation; sedimentary petrology; environment; glaciology; geomorphology; geochemistry; sedimentary structures; Cape Colombier; bedding plane irregularities</ED>
<EG>Phanerozoic; carbonate rocks; sedimentary rocks; Canada; North America; upper Quaternary; Quaternary</EG>
<SD>C 14; Cenozoico; Medio litoral; Dolomía; Canadá Este; Bloque errático; Colada; Transporte glaciar; Holoceno; Isótopo; Holoceno inf; Quebec; Isótopo radioactivo; Estuario San Lorenzo; Estriación; Geocronología; Estratigrafía; Sedimentación; Petrología roca sedimentaria; Medio; Geomorfología; Geoquímica; Estructura sedimentaria</SD>
<LO>AGI</LO>
<ID>03-0360252</ID>
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