Origins and fates of H2S in the Cambrian and Ordovician in Tazhong area: Evidence from sulfur isotopes, fluid inclusions and production data
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- 作者：Chunfang Caia ; b ; cai_cf@mail.iggcas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Guoyi Huc ; HongXia Lia ; Lei Jianga ; Wenxiang Heb ; Baoshou Zhangd ; Lianqi Jiaa ; Tiankai Wanga
- 关键词：TSR ; H2S ; Oil ; Methane ; Sulfur isotope ; Carbon isotope ; Tarim Basin
- 刊名：Marine and Petroleum Geology
- 出版年：2015
- 出版时间：November 2015
- 年：2015
- 卷：67
- 期：Complete
- 页码：408-418
- 全文大小：2222 K
文摘
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The H2S was derived from TSR, and diluted by late charged H2S-poor dry gas.
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Significant amounts of H2S were contributed from exsolution from water during production.
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A significant amount of H2S was incorporated into oils and solid bitumen.
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H2S concentrations cannot reflect TSR degrees in the area.
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