鄂尔多斯盆地东北部上古生界煤系烃源岩17&alpha;(H)-重排藿烷类的分布及成因探讨

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鄂尔多斯盆地东北部上古生界煤系烃源岩17α(H)-重排藿烷类的分布及成因探讨

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中图分类号: P618.130.1

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Origin of 17α (H)-Rearranged Hopanes in Upper Palaeozoic Coal Bearing Source Rocks in Northeast Ordos Basin

摘要

摘要: 鄂尔多斯盆地东北部上古生界10个典型煤系烃源岩样品中检测出三类重排藿烷，分别为17α(H)-重排藿烷、18α(H)-新藿烷以及未知结构的早洗脱重排藿烷。烃源岩样品中藿烷类具有两种分布型式：①以C₃₀藿烷为主峰的C₂₇~C₃₅(缺C₂₈)藿烷类常规分布型式，含少量17α (H)-重排藿烷和18α(H)-新藿烷；②以富含17α(H)-重排藿烷和C₃₀早洗脱重排藿烷为特征。含有高~异常高相对丰度17α(H)-重排藿烷的烃源岩样品，其17α(H)-重排藿烷的绝对浓度也明显较高。从烃源岩生源构成、有机质丰度及其赋存状态、成熟度以及沉积与成岩环境4个方面探讨了高丰度17α(H)-重排藿烷的成因。研究结果表明，烃源岩中高丰度的17α(H)-重排藿烷的形成与高等植物生源有一定联系、亚氧化—氧化的扇缘泥炭沼泽相是形成高~异常高丰度17α(H)-重排藿烷的有利沉积相带；而烃源岩显微组分、有机质丰度及其赋存状态以及有机质成熟度的影响尚不确定。
- 鄂尔多斯盆地 /
- 煤系烃源岩 /
- 17&alpha /
- (H)-重排藿烷 /
- 生源构成 /
- 沉积环境
Abstract: Geochemical characteristics of saturated hydrocarbons have been discussed on the basis of GC/MS analysis for the 10 typical coal-bearing source rock samples in northeast Ordos Basin. Three series of rearranged hopanes, 17α (H)-diahopanes, 18α (H)-neohopanes and unidentified earlyeluting rearranged hopanes, were detected. The analytical results showed that the hopane series compounds have two different distribution patterns. One is conventional pattern, which has high abundance of regular hopanes, low abundance of 17α (H)-diahopanes and 18α (H)-neohopanes, represented by source rock samples from Yu 20 and Shuang 1 well. The other one is unconventional model, characterized by abnormally rich in 17α (H)-diahopanes and a C₃₀-early-eluting rearranged hopane, represented by source rock samples from Su 27 well. The source rocks from Su 27 well high relative abundance of 17α (H)-diahopanes and also high absolute concentration. The main controlling factors of extremely abundant 17α (H)-diahopanes are discussed from the composition of organic materials, maceral, the abundance of organic matters and its occurrence, maturity, depositional and diagenetic environment. The result shows that the origin and accumulation of high abundance of 17α (H)-diahopanes in source rocks has a close relationship with higher plants source materials. Weak oxidation to oxidation fan marginal peat bog facies is a favorable sedimentary facies for forming a significant proportion of 17α (H)-diahopanes. However, the influences of maceral, maturity, the abundance of organic matters and its occurrence are not sure.
- Ordos Basin /
- coal-bearing source rocks /
- 17&alpha /
- (H)-diahopane /
- composition of organic materials /
- depositional environment

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[1]	张治波, 徐颖, 苗艳菊, 王文锋, 赵迪斐, 陈丹玲. 昌都盆地古近系贡觉组物源及其沉积环境 . 沉积学报, 2022, 40(6): 1561-1581. doi: 10.14027/j.issn.1000-0550.2022.094
[2]	郭沫贞, 吕福亮, 邵大力, 侯福斗, 杨涛涛, 李东. 东爪哇盆地抱球虫灰岩遗迹化石及其沉积环境分析 . 沉积学报, 2021, 39(3): 713-722. doi: 10.14027/j.issn.1000-0550.2020.028
[3]	袁灵聪, 朱晓军, 蔡进功, 钟锴. 东海盆地长江坳陷美人峰组烃源岩沉积环境与生烃潜力评价 . 沉积学报, 2021, 39(2): 506-514. doi: 10.14027/j.issn.1000-0550.2020.016
[4]	李森, 朱如凯, 崔景伟, 罗忠, 焦航, 柳涵. 鄂尔多斯盆地长7段细粒沉积岩特征与古环境——以铜川地区瑶页1井为例 . 沉积学报, 2020, 38(3): 554-570. doi: 10.14027/j.issn.1000-0550.2019.062
[5]	刘福田, 李荣西, 刘新社, 杨鸣一, 赵帮胜, 吴小力, 覃小丽. 鄂尔多斯盆地苏里格西部气田“源控”主导的天然气成藏研究 . 沉积学报, 2019, 37(6): 1129-1139. doi: 10.14027/j.issn.1000-0550.2019.052
[6]	贾浪波, 钟大康, 孙海涛, 严锐涛, 张春林, 莫午零, 邱存, 董媛, 李兵, 廖广新. 鄂尔多斯盆地本溪组沉积物物源探讨及其构造意义 . 沉积学报, 2019, 37(5): 1087-1103. doi: 10.14027/j.issn.1000-0550.2019.014
[7]	王成, 王万春, 王建丰, 樊海龙. 鄂尔多斯盆地奥陶系烃源岩支链烷烃特征及其地质意义 . 沉积学报, 2017, 35(4): 853-862. doi: 10.14027/j.cnki.cjxb.2017.04.019
[8]	王峰, 刘玄春, 邓秀芹, 李元昊, 田景春, 李士祥, 尤靖茜. 鄂尔多斯盆地纸坊组微量元素地球化学特征及沉积环境指示意义 . 沉积学报, 2017, 35(6): 1265-1273. doi: 10.14027/j.cnki.cjxb.2017.06.017
[9]	张春良, 沈玉林, 秦勇, 赵志刚, 杨柳, 谢国梁. 崖南凹陷Y1井崖三段煤系烃源岩发育规律 . 沉积学报, 2016, 34(5): 1003-1010. doi: 10.14027/j.cnki.cjxb.2016.05.019
[10]	李红磊, 张敏, 姜连, 程熊. 利用芳烃参数研究煤系烃源岩中重排藿烷成因 . 沉积学报, 2016, 34(1): 191-199. doi: 10.14027/j.cnki.cjxb.2016.01.018
[11]	赵俊峰, 屈红军, 林晋炎, 刘祥, 杨扬, 林川. 湖泊三角洲沉积露头精细解剖——以鄂尔多斯盆地裴庄剖面为例 . 沉积学报, 2014, 32(6): 1026-1034.
[12]	刘群, 袁选俊, 林森虎, 王岚, 郭浩, 潘松圻, 姚泾利. 鄂尔多斯盆地延长组湖相黏土岩分类和沉积环境探讨 . 沉积学报, 2014, 32(6): 1016-1025.
[13]	. 鄂尔多斯盆地余兴庄—子洲地区上古生界山3 2储层砂岩成岩作用与成岩相 . 沉积学报, 2011, 29(6): 1031-1040.
[14]	. 鄂尔多斯盆地延长组长10期沉积环境与沉积体系 . 沉积学报, 2011, 29(6): 1105-1114.
[15]	叶黎明. 鄂尔多斯盆地东部山西组海相沉积环境分析 . 沉积学报, 2008, 26(2): 202-210.
[16]	胡平. 准噶尔盆地东部侏罗纪含煤岩系沉积环境及基准面旋回划分 . 沉积学报, 2006, 24(3): 378-386.
[17]	邵磊, 李文厚, 袁明生. 吐鲁番—哈密盆地陆源碎屑沉积环境及物源分析 . 沉积学报, 1999, 17(3): 435-442.
[18]	戴卿林, 郝石生, 盛国英, 傅家谟. 吐哈盆地侏罗纪煤系源岩芳烃组成及生源、环境意义 . 沉积学报, 1997, 15(2): 198-201.
[19]	赵孟为, Hans Ahrendt, Klaus Wem mer. K－Ar测年法在确定沉积岩成岩时代中的应用——以鄂尔多斯盆地为例 . 沉积学报, 1996, 14(3): 11-21.
[20]	肖贤明, 刘德汉, 傅家谟. 我国聚煤盆地煤系烃源岩生烃评价与成烃模式 . 沉积学报, 1996, 14(S1): 10-17.

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鄂尔多斯盆地东北部上古生界煤系烃源岩17α(H)-重排藿烷类的分布及成因探讨

刊出日期: 2014-08-10

中图分类号: P618.130.1

关键词:

17&alpha /

摘要: 鄂尔多斯盆地东北部上古生界10个典型煤系烃源岩样品中检测出三类重排藿烷，分别为17α(H)-重排藿烷、18α(H)-新藿烷以及未知结构的早洗脱重排藿烷。烃源岩样品中藿烷类具有两种分布型式：①以C₃₀藿烷为主峰的C₂₇~C₃₅(缺C₂₈)藿烷类常规分布型式，含少量17α (H)-重排藿烷和18α(H)-新藿烷；②以富含17α(H)-重排藿烷和C₃₀早洗脱重排藿烷为特征。含有高~异常高相对丰度17α(H)-重排藿烷的烃源岩样品，其17α(H)-重排藿烷的绝对浓度也明显较高。从烃源岩生源构成、有机质丰度及其赋存状态、成熟度以及沉积与成岩环境4个方面探讨了高丰度17α(H)-重排藿烷的成因。研究结果表明，烃源岩中高丰度的17α(H)-重排藿烷的形成与高等植物生源有一定联系、亚氧化—氧化的扇缘泥炭沼泽相是形成高~异常高丰度17α(H)-重排藿烷的有利沉积相带；而烃源岩显微组分、有机质丰度及其赋存状态以及有机质成熟度的影响尚不确定。

Origin of 17α (H)-Rearranged Hopanes in Upper Palaeozoic Coal Bearing Source Rocks in Northeast Ordos Basin

Publish Date: 2014-08-10

Keywords:

Abstract: Geochemical characteristics of saturated hydrocarbons have been discussed on the basis of GC/MS analysis for the 10 typical coal-bearing source rock samples in northeast Ordos Basin. Three series of rearranged hopanes, 17α (H)-diahopanes, 18α (H)-neohopanes and unidentified earlyeluting rearranged hopanes, were detected. The analytical results showed that the hopane series compounds have two different distribution patterns. One is conventional pattern, which has high abundance of regular hopanes, low abundance of 17α (H)-diahopanes and 18α (H)-neohopanes, represented by source rock samples from Yu 20 and Shuang 1 well. The other one is unconventional model, characterized by abnormally rich in 17α (H)-diahopanes and a C₃₀-early-eluting rearranged hopane, represented by source rock samples from Su 27 well. The source rocks from Su 27 well high relative abundance of 17α (H)-diahopanes and also high absolute concentration. The main controlling factors of extremely abundant 17α (H)-diahopanes are discussed from the composition of organic materials, maceral, the abundance of organic matters and its occurrence, maturity, depositional and diagenetic environment. The result shows that the origin and accumulation of high abundance of 17α (H)-diahopanes in source rocks has a close relationship with higher plants source materials. Weak oxidation to oxidation fan marginal peat bog facies is a favorable sedimentary facies for forming a significant proportion of 17α (H)-diahopanes. However, the influences of maceral, maturity, the abundance of organic matters and its occurrence are not sure.

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鄂尔多斯盆地东北部上古生界煤系烃源岩17α(H)-重排藿烷类的分布及成因探讨

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Origin of 17α (H)-Rearranged Hopanes in Upper Palaeozoic Coal Bearing Source Rocks in Northeast Ordos Basin

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鄂尔多斯盆地东北部上古生界煤系烃源岩17α(H)-重排藿烷类的分布及成因探讨

English Abstract

Origin of 17α (H)-Rearranged Hopanes in Upper Palaeozoic Coal Bearing Source Rocks in Northeast Ordos Basin

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鄂尔多斯盆地东北部上古生界煤系烃源岩17α(H)-重排藿烷类的分布及成因探讨

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Origin of 17α (H)-Rearranged Hopanes in Upper Palaeozoic Coal Bearing Source Rocks in Northeast Ordos Basin

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出版历程

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鄂尔多斯盆地东北部上古生界煤系烃源岩17α(H)-重排藿烷类的分布及成因探讨

English Abstract

Origin of 17α (H)-Rearranged Hopanes in Upper Palaeozoic Coal Bearing Source Rocks in Northeast Ordos Basin

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期刊在线

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