Late Paleoproterozoic rift-related magmatic rocks in the North China Craton: Geological records of rifting in the Columbia supercontinent
Late Paleoproterozoic (1.84‒1.62Ga) magmatic rocks including dykes/sills/intrusions and volcanic rocks occur throughout the North China Craton (NCC), which is considered to be part of the Columbia supercontinent by ca. 1.9–1.85Ga. On the basis of petrogeochemical data, these magmatic rocks can be cl...
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| Veröffentlicht in: | Earth-science reviews 2013-10, Vol.125, p.69-86 |
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| creator | Xia, Linqi Xia, Zuchun Xu, Xueyi Li, Xiangmin Ma, Zhongping |
| description | Late Paleoproterozoic (1.84‒1.62Ga) magmatic rocks including dykes/sills/intrusions and volcanic rocks occur throughout the North China Craton (NCC), which is considered to be part of the Columbia supercontinent by ca. 1.9–1.85Ga. On the basis of petrogeochemical data, these magmatic rocks can be classified into three major magma types: HN (Nb/La>0.8, Ce/Nb=1.7‒3, (Th/Nb)N=0.6‒1.2), MN (Nb/La=0.8–0.5, Ce/Nb=3‒5, (Th/Nb)N=0.9‒3.5) and LN (Nb/La |
| doi_str_mv | 10.1016/j.earscirev.2013.06.004 |
| format | Article |
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On the basis of petrogeochemical data, these magmatic rocks can be classified into three major magma types: HN (Nb/La>0.8, Ce/Nb=1.7‒3, (Th/Nb)N=0.6‒1.2), MN (Nb/La=0.8–0.5, Ce/Nb=3‒5, (Th/Nb)N=0.9‒3.5) and LN (Nb/La<0.5, Ce/Nb=5‒80, (Th/Nb)N=1‒60). The geochemical variation of the MN and LN rocks can be explained by lithospheric contamination of asthenosphere- (or plume-) derived magmas, whereas the parental magmas of the HN rocks did not undergo, during their ascent, pronounced lithospheric contamination. These magmatic rocks exhibit at least two characteristics: (1) most displaying a spectrum of compositions from mafic to silicic; (2) forming in an intracontinental rift setting. This Late Paleoproterozoic rift-related magmatism is the most distinguishing feature of the rifting of the Columbia supercontinent.</description><identifier>ISSN: 0012-8252</identifier><identifier>EISSN: 1872-6828</identifier><identifier>DOI: 10.1016/j.earscirev.2013.06.004</identifier><identifier>CODEN: ESREAV</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>China ; Columbia supercontinent ; Contamination ; Continental rift ; Cratons ; Dyke swarm ; Geochemistry ; Geological time ; Igneous rocks ; Intrusion ; Late Paleoproterozoic ; Lithosphere ; Magma ; Niobium ; North China Craton ; Rocks ; volcanic rocks ; Volcanism ; Volcanoes</subject><ispartof>Earth-science reviews, 2013-10, Vol.125, p.69-86</ispartof><rights>2013 Elsevier B.V.</rights><rights>Copyright Elsevier Sequoia S.A. Oct 2013</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a423t-121d26e480ca501b247e2bd21a0437f8b3f06cb29aa070b1898d6d9272e253dd3</citedby><cites>FETCH-LOGICAL-a423t-121d26e480ca501b247e2bd21a0437f8b3f06cb29aa070b1898d6d9272e253dd3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0012825213001177$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65306</link.rule.ids></links><search><creatorcontrib>Xia, Linqi</creatorcontrib><creatorcontrib>Xia, Zuchun</creatorcontrib><creatorcontrib>Xu, Xueyi</creatorcontrib><creatorcontrib>Li, Xiangmin</creatorcontrib><creatorcontrib>Ma, Zhongping</creatorcontrib><title>Late Paleoproterozoic rift-related magmatic rocks in the North China Craton: Geological records of rifting in the Columbia supercontinent</title><title>Earth-science reviews</title><description>Late Paleoproterozoic (1.84‒1.62Ga) magmatic rocks including dykes/sills/intrusions and volcanic rocks occur throughout the North China Craton (NCC), which is considered to be part of the Columbia supercontinent by ca. 1.9–1.85Ga. On the basis of petrogeochemical data, these magmatic rocks can be classified into three major magma types: HN (Nb/La>0.8, Ce/Nb=1.7‒3, (Th/Nb)N=0.6‒1.2), MN (Nb/La=0.8–0.5, Ce/Nb=3‒5, (Th/Nb)N=0.9‒3.5) and LN (Nb/La<0.5, Ce/Nb=5‒80, (Th/Nb)N=1‒60). The geochemical variation of the MN and LN rocks can be explained by lithospheric contamination of asthenosphere- (or plume-) derived magmas, whereas the parental magmas of the HN rocks did not undergo, during their ascent, pronounced lithospheric contamination. These magmatic rocks exhibit at least two characteristics: (1) most displaying a spectrum of compositions from mafic to silicic; (2) forming in an intracontinental rift setting. This Late Paleoproterozoic rift-related magmatism is the most distinguishing feature of the rifting of the Columbia supercontinent.</description><subject>China</subject><subject>Columbia supercontinent</subject><subject>Contamination</subject><subject>Continental rift</subject><subject>Cratons</subject><subject>Dyke swarm</subject><subject>Geochemistry</subject><subject>Geological time</subject><subject>Igneous rocks</subject><subject>Intrusion</subject><subject>Late Paleoproterozoic</subject><subject>Lithosphere</subject><subject>Magma</subject><subject>Niobium</subject><subject>North China Craton</subject><subject>Rocks</subject><subject>volcanic rocks</subject><subject>Volcanism</subject><subject>Volcanoes</subject><issn>0012-8252</issn><issn>1872-6828</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNqFkU2O1DAQhSMEEs3AGcYSGzYJZefPYTeKYEBqARLM2qrYlW43SdzYzkhwA26NQwMLNmxs2fW95yq_LLvmUHDgzctTQeiDtp7uCwG8LKApAKoH2Y7LVuSNFPJhtgPgIpeiFo-zJyGcIJ2ha3fZjz1GYh9xInf2LpJ3353VzNsx5p6mVDRsxsOMcbt1-ktgdmHxSOy98_HI-qNdkPUeo1tesVtykztYjRPzpJ03gbnxl5ldDn-EvZvWebDIwnomr92SirTEp9mjEadAz37vV9ndm9ef-7f5_sPtu_5mn2MlyphzwY1oqJKgsQY-iKolMRjBEaqyHeVQjtDoQXSI0MLAZSdNYzrRChJ1aUx5lb24-KZ5v64Uoppt0DRNuJBbg-JNzcuuKUWX0Of_oCe3-iV1p3hVCQltzXmi2gulvQvB06jO3s7ovykOaotIndTfiNQWkYJGpYiS8vqiHNEpPHgb1N2nBNQA2yo34uZCUPqRe0teJRtaNJlkpqMyzv73lZ-Jiqj7</recordid><startdate>20131001</startdate><enddate>20131001</enddate><creator>Xia, Linqi</creator><creator>Xia, Zuchun</creator><creator>Xu, Xueyi</creator><creator>Li, Xiangmin</creator><creator>Ma, Zhongping</creator><general>Elsevier B.V</general><general>Elsevier Sequoia S.A</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope></search><sort><creationdate>20131001</creationdate><title>Late Paleoproterozoic rift-related magmatic rocks in the North China Craton: Geological records of rifting in the Columbia supercontinent</title><author>Xia, Linqi ; Xia, Zuchun ; Xu, Xueyi ; Li, Xiangmin ; Ma, Zhongping</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a423t-121d26e480ca501b247e2bd21a0437f8b3f06cb29aa070b1898d6d9272e253dd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>China</topic><topic>Columbia supercontinent</topic><topic>Contamination</topic><topic>Continental rift</topic><topic>Cratons</topic><topic>Dyke swarm</topic><topic>Geochemistry</topic><topic>Geological time</topic><topic>Igneous rocks</topic><topic>Intrusion</topic><topic>Late Paleoproterozoic</topic><topic>Lithosphere</topic><topic>Magma</topic><topic>Niobium</topic><topic>North China Craton</topic><topic>Rocks</topic><topic>volcanic rocks</topic><topic>Volcanism</topic><topic>Volcanoes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Xia, Linqi</creatorcontrib><creatorcontrib>Xia, Zuchun</creatorcontrib><creatorcontrib>Xu, Xueyi</creatorcontrib><creatorcontrib>Li, Xiangmin</creatorcontrib><creatorcontrib>Ma, Zhongping</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Earth-science reviews</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Xia, Linqi</au><au>Xia, Zuchun</au><au>Xu, Xueyi</au><au>Li, Xiangmin</au><au>Ma, Zhongping</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Late Paleoproterozoic rift-related magmatic rocks in the North China Craton: Geological records of rifting in the Columbia supercontinent</atitle><jtitle>Earth-science reviews</jtitle><date>2013-10-01</date><risdate>2013</risdate><volume>125</volume><spage>69</spage><epage>86</epage><pages>69-86</pages><issn>0012-8252</issn><eissn>1872-6828</eissn><coden>ESREAV</coden><abstract>Late Paleoproterozoic (1.84‒1.62Ga) magmatic rocks including dykes/sills/intrusions and volcanic rocks occur throughout the North China Craton (NCC), which is considered to be part of the Columbia supercontinent by ca. 1.9–1.85Ga. On the basis of petrogeochemical data, these magmatic rocks can be classified into three major magma types: HN (Nb/La>0.8, Ce/Nb=1.7‒3, (Th/Nb)N=0.6‒1.2), MN (Nb/La=0.8–0.5, Ce/Nb=3‒5, (Th/Nb)N=0.9‒3.5) and LN (Nb/La<0.5, Ce/Nb=5‒80, (Th/Nb)N=1‒60). The geochemical variation of the MN and LN rocks can be explained by lithospheric contamination of asthenosphere- (or plume-) derived magmas, whereas the parental magmas of the HN rocks did not undergo, during their ascent, pronounced lithospheric contamination. These magmatic rocks exhibit at least two characteristics: (1) most displaying a spectrum of compositions from mafic to silicic; (2) forming in an intracontinental rift setting. This Late Paleoproterozoic rift-related magmatism is the most distinguishing feature of the rifting of the Columbia supercontinent.</abstract><cop>Amsterdam</cop><pub>Elsevier B.V</pub><doi>10.1016/j.earscirev.2013.06.004</doi><tpages>18</tpages></addata></record> |
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| subjects | China Columbia supercontinent Contamination Continental rift Cratons Dyke swarm Geochemistry Geological time Igneous rocks Intrusion Late Paleoproterozoic Lithosphere Magma Niobium North China Craton Rocks volcanic rocks Volcanism Volcanoes |
| title | Late Paleoproterozoic rift-related magmatic rocks in the North China Craton: Geological records of rifting in the Columbia supercontinent |
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