浙江省上震旦统和古生界烃源岩演化程度研究
he evolutive degree of the source rock of the Upper Sinianand the Paleozoic of Zhejiang province
浙江省烃源岩主要有两套：一套是盆地基底海相地层，另一套是内陆盆地相地层。其中海相地层中的主力烃源岩层为上震旦统和上古生界石炭—二叠系。本文以镜质体反射率、热解、牙形刺、孢粉作为划分的主要依据，来研究金衢盆地上震旦统和古生界烃源岩的演化程度。
he source rock of Zhejiang province mainly has two set:one set is the stratum of marine facies of the basin base,the other is the stratum of the inland basin.The stratum of main source rock among the marine facies is the Upper Sinian and the Paleozoic group.The content of this text is studying evolutive degree of the source rock of the Upper Sinian and the Paleozoic group mainly by vitrinite,pyrogenation,conodont and sporopollen.
袁续祖、王明磊、张廷山、郑华平
石油天然气地质、石油天然气勘探
烃源岩演化程度浙江省
source rock evolutive degree Zhejiang province
袁续祖,王明磊,张廷山,郑华平.浙江省上震旦统和古生界烃源岩演化程度研究[EB/OL].(2006-02-09)[2025-08-24].http://www.paper.edu.cn/releasepaper/content/200602-44.点此复制
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