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

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名

邮箱

手机号码

标题

留言内容

验证码

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

详细信息

中图分类号: P618.130.1

计量

文章访问数: 1546
HTML全文浏览量: 63
PDF下载量: 1001
被引次数: 0

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

HTML全文

参考文献(0)

[1]	白莹, 马占荣, 黄正良, 闫伟, 高建荣, 赵振宇. 鄂尔多斯盆地西缘奥陶系乌拉力克组混积岩岩相类型及沉积模式 . 沉积学报, 2025, 43(4): 1213-1232. doi: 10.14027/j.issn.1000-0550.2024.120
[2]	张文俊, 林舒敏, 柯行, 张敏. 煤系烃源岩中四种类型高丰度重排藿烷组成特征及成因探讨——以鄂尔多斯盆地上古生界为例 . 沉积学报, 2025, 43(2): 683-700. doi: 10.14027/j.issn.1000-0550.2024.028
[3]	王晓琳, 朱筱敏, 赖锦, 王贵文, 李红斌. 铝土岩系沉积环境及储层特征——以鄂尔多斯盆地临兴地区本溪组为例 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.110
[4]	宋慧波, 张彬, 于振锋, 金毅, 胡斌, 牛永斌, 张立军. 鄂尔多斯盆地东缘太原组风暴沉积特征及环境模式 . 沉积学报, 2024, 42(4): 1370-1383. doi: 10.14027/j.issn.1000-0550.2023.020
[5]	李俊, 赵红格, 汪建, 郭惠, 邵晓州. 鄂尔多斯盆地西缘中部三叠系延长组碎屑岩沉积环境及物源示踪 . 沉积学报, 2024, 42(5): 1621-1638. doi: 10.14027/j.issn.1000-0550.2022.120
[6]	林舒敏, 张敏, 李洪波. 鄂尔多斯盆地上古生界煤系烃源岩三环萜烷成因探讨 . 沉积学报, 2024, 42(4): 1433-1446. doi: 10.14027/j.issn.1000-0550.2023.139
[7]	林舒敏, 张敏, 李洪波. 鄂尔多斯盆地上古生界煤系烃源岩三环萜烷成因探讨 . 沉积学报, 2024, (): -.
[8]	张云望, 金鑫, 乔培军, 李滨兵, 洪彦哲, 陈俞超, 芦刚, 杜怡星, 时志强. 鄂尔多斯盆地东北部下侏罗统富县组沉积物源分析 . 沉积学报, 2023, 41(5): 1414-1429. doi: 10.14027/j.issn.1000-0550.2022.154
[9]	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
[10]	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
[11]	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
[12]	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
[13]	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
[14]	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
[15]	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.
[16]	. 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.
[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.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 1546
HTML全文浏览量: 63
PDF下载量: 1001
被引次数: 0

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.

留言板

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

计量

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

计量

目录

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

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

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

计量

出版历程

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

计量

出版历程

目录

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

全文HTML

目录

友情链接

期刊在线

联系我们