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- W3148230892 abstract "含碳的来源岩石由在 Santanghu 钻识别了() 盆为他们的来源潜力，采用的器官的地球化学和 RockEval 热分解被评估。有机物起源和这些样品的 depositional 环境也通过 biomarker 分析被决定。大多数在 Santanghu 盆的含碳的来源岩石被内容和高可引出的有机物内容和烃产出的全部的器官的碳(TOC ) 的高价值描述，显示他们是有高油的器官富人的来源岩石生产潜力。有机物是主要打字我和有类型 III kerogen 的次要的贡献的类型 II kerogen 由它的热分解参数和碳同位素价值示威了。根据 Ro (%) 和 T 最大价值，大多数学习样品在早 -- 到中间热的成熟舞台；仅仅样品的一些在一个高度成熟的阶段(过去的山峰油产生) 。biomarker 分析揭示海藻 / 细菌的有机物输入的优势，与陆地植物材料的次要的贡献。Pr/Ph 比率支持一个 suboxic depositional 条件，与前辈建议的浅海或海洋大陆人的轮流出现的环境一致。" @default.
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- W3148230892 date "2013-01-01" @default.
- W3148230892 modified "2023-09-28" @default.
- W3148230892 title "Source Rock Potential and Organic Geochemistry of Carboniferous Source Rocks in Santanghu Basin, NW China" @default.
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