Physical condition favoring formation of marine hydrocarbon source rocks
Both tremendous productivity and anoxic condition favor formation of marine hydrocarbon source rocks. The anoxic condition could be realized in the marginal seas by a physical process-water mass delamination. For example, differences in salinity and temperature separated water mass into two layers i...
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Veröffentlicht in: | Dizhi kexue 2011-01, Vol.46 (1), p.1-4 |
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description | Both tremendous productivity and anoxic condition favor formation of marine hydrocarbon source rocks. The anoxic condition could be realized in the marginal seas by a physical process-water mass delamination. For example, differences in salinity and temperature separated water mass into two layers in the Red Sea. Such a case might occur also in the Paleozoic South China. The anoxic condition in the deep layer is favorable for accumulation of marine hydrocarbon source rocks. |
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The anoxic condition could be realized in the marginal seas by a physical process-water mass delamination. For example, differences in salinity and temperature separated water mass into two layers in the Red Sea. Such a case might occur also in the Paleozoic South China. The anoxic condition in the deep layer is favorable for accumulation of marine hydrocarbon source rocks.</description><identifier>ISSN: 0563-5020</identifier><language>chi</language><subject>China ; Hydrocarbons ; Marine ; Productivity ; Red Sea ; Rocks ; Salinity ; Seas</subject><ispartof>Dizhi kexue, 2011-01, Vol.46 (1), p.1-4</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784</link.rule.ids></links><search><creatorcontrib>Liu, Guangding</creatorcontrib><creatorcontrib>Yang, Changchun</creatorcontrib><creatorcontrib>Wang, Qingchen</creatorcontrib><title>Physical condition favoring formation of marine hydrocarbon source rocks</title><title>Dizhi kexue</title><description>Both tremendous productivity and anoxic condition favor formation of marine hydrocarbon source rocks. The anoxic condition could be realized in the marginal seas by a physical process-water mass delamination. For example, differences in salinity and temperature separated water mass into two layers in the Red Sea. Such a case might occur also in the Paleozoic South China. The anoxic condition in the deep layer is favorable for accumulation of marine hydrocarbon source rocks.</description><subject>China</subject><subject>Hydrocarbons</subject><subject>Marine</subject><subject>Productivity</subject><subject>Red Sea</subject><subject>Rocks</subject><subject>Salinity</subject><subject>Seas</subject><issn>0563-5020</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNqFjL1OwzAURj2ARFX6Dh5ZIvn6xk48ogooUiUYylzd-IdaJHGxE6S-PRGwM336jo7OFVsJpbFSQoobtikldkKAkqhrvWK719OlREs9t2l0cYpp5IG-Uo7jOw8pD_SDUuADLczz08XlZCl3Cy1pztbz5X-UW3YdqC9-87dr9vb4cNjuqv3L0_P2fl-dAfVUSdIKoW0NOu-hEwZcLSQF6W2oUTYAGNAo22AwXodOBdV2ZB2QE3op4Jrd_XbPOX3OvkzHIRbr-55Gn-ZyBG1kLQxC878qEFCq2mj8Bk6gWKM</recordid><startdate>20110101</startdate><enddate>20110101</enddate><creator>Liu, Guangding</creator><creator>Yang, Changchun</creator><creator>Wang, Qingchen</creator><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20110101</creationdate><title>Physical condition favoring formation of marine hydrocarbon source rocks</title><author>Liu, Guangding ; Yang, Changchun ; Wang, Qingchen</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p136t-2a65318893dee1b091d402af2ecf4327113f395c73f9e6fb5f58bacd1ad061363</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi</language><creationdate>2011</creationdate><topic>China</topic><topic>Hydrocarbons</topic><topic>Marine</topic><topic>Productivity</topic><topic>Red Sea</topic><topic>Rocks</topic><topic>Salinity</topic><topic>Seas</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Guangding</creatorcontrib><creatorcontrib>Yang, Changchun</creatorcontrib><creatorcontrib>Wang, Qingchen</creatorcontrib><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Dizhi kexue</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Guangding</au><au>Yang, Changchun</au><au>Wang, Qingchen</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Physical condition favoring formation of marine hydrocarbon source rocks</atitle><jtitle>Dizhi kexue</jtitle><date>2011-01-01</date><risdate>2011</risdate><volume>46</volume><issue>1</issue><spage>1</spage><epage>4</epage><pages>1-4</pages><issn>0563-5020</issn><abstract>Both tremendous productivity and anoxic condition favor formation of marine hydrocarbon source rocks. The anoxic condition could be realized in the marginal seas by a physical process-water mass delamination. For example, differences in salinity and temperature separated water mass into two layers in the Red Sea. Such a case might occur also in the Paleozoic South China. The anoxic condition in the deep layer is favorable for accumulation of marine hydrocarbon source rocks.</abstract><tpages>4</tpages></addata></record> |
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subjects | China Hydrocarbons Marine Productivity Red Sea Rocks Salinity Seas |
title | Physical condition favoring formation of marine hydrocarbon source rocks |
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