塔里木盆地下寒武统泥质烃源岩成烃生物组合的构造-沉积环境控制因素

doi:10.11743/ogg20140514

石油与天然气地质 ›› 2014, Vol. 35 ›› Issue (5): 685-695.doi: 10.11743/ogg20140514

塔里木盆地下寒武统泥质烃源岩成烃生物组合的构造-沉积环境控制因素

胡广^1,2,3, 刘文汇^2,3, 腾格尔^2,3, 陈强路^2,3, 谢小敏^2,3, 王杰^2,3, 卢龙飞^2,3, 申宝剑^2,3

1. 同济大学海洋与地球科学学院, 上海 200092;
2. 中国石化油气成藏重点实验室, 江苏无锡 214126;
3. 中国石化石油勘探开发研究院无锡石油地质研究所, 江苏无锡 214151

收稿日期:2014-04-11 修回日期:2014-08-12 出版日期:2014-10-08 发布日期:2014-10-17
通讯作者: 刘文汇（1957- ），男，博士、教授，天然气地质学及油气地球化学。E-mail：whliu.syky@sinopec.com。 E-mail:whliu.syky@sinopec.com
第一作者简介:胡广（1978- ），男，博士、工程师，石油地质。E-mail：guanghu1198119@163.com。
基金项目:
国家重点基础研究发展计划（“973”计划）项目（2012CB214801）。

Tectonic-sedimentary constrains for hydrocarbon generating organism assemblage in the Lower Cambrian argillaceous source rocks, Tarim Basin

Hu Guang^1,2,3, Liu Wenhui^2,3, Tengger^2,3, Cheng Qianglu^2,3, Xie Xiaomin^2,3, Wang Jie^2,3, Lu Longfei^2,3, Shen Baojian^2,3

1. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China;
2. Key Laboratory of Petroleum Accumulation Mechanisms, SINOPEC, Wuxi, Jiangsu 214151, China;
3. Wuxi Research Institute of Petroleum Geology, SINOPEC Exploration & Production Research Institute, Wuxi, Jiangsu 214151, China

Received:2014-04-11 Revised:2014-08-12 Online:2014-10-08 Published:2014-10-17

摘要/Abstract

摘要：

成烃生物组合是烃源岩研究的重要内容，目前关于成烃生物研究主要集中在生烃模拟实验，对成烃生物发育的地质控制因素研究在油气地质界还相对较少，然而这方面的研究是利用成烃生物预测优质烃源岩分布并指导油气勘探的重要环节。成烃生物面貌的研究结果表明，西山布拉克组和玉尔吐斯组主要以底栖藻为主，含浮游藻类，但西山布拉克组主要以底栖藻类和浮游藻类为主，而东二沟剖面玉尔吐斯组则以底栖藻类（红藻）为主。稀土元素地球化学揭示西山布拉克组和玉尔吐斯组沉积时均受热水作用影响，且西山布拉克组受影响程度要强于玉尔吐斯组。泥岩稀土、主量和微量元素分析发现，西山布拉克组和玉尔吐斯组均为还原环境，但西山布拉克组水体还原性强度要弱，水动力条件稍强，活跃的火山活动使得库鲁克塔格地区西山布拉克组沉积期古地貌起伏程度要强于柯坪地区。对比现代藻类分布模式，构造活动、水体深度以及古地貌上差异可能是导致南雅尔当山剖面西山布拉克组和东二沟剖面玉尔吐斯组成烃生物面貌不同的重要原因。

关键词: 成烃生物组合, 烃源岩, 玉尔吐斯组, 西山布拉克组, 下寒武统, 塔里木盆地

Abstract:

Hydrocarbon generating organism is an important object for the source rock research.The studies,so far,were focused on their hydrocarbon-generation potential via simulation experiments,and less attention was paid to the geological settings that affect development and distribution of hydrocarbon generating organisms.However,the development and distribution of hydrocarbon generating organisms is very important for predicting source rocks and guiding petroleum exploration.In this study,the Lower Cambrian Xishanbulake and Yuertus formations were selected from the Southern Yaerdangshan and Dongergou sections in Kuluketage and Keping districts,respectively.Researches on two formations demonstrate that the hydrocarbon generating organisms in the Xishanbulake Formation are dominated by benthic algae,and include some planktonic algae;whereas hydrocarbon generating organisms in the Yuertusi Formation are benthic algae.Anomaly of elements Ce and Eu and REE patterns of cherts in the two formations imply that the two sections were affected by hydrothermal fluid,and that the influence in the Southern Yaerdangshan section was stronger than that in the Dongergou section.Major and trace elements analyses of mudstones indicate that the Xishanbulake Formation have less reduction water,and more active volcano in the Kuluketage district which might be resulted in more undulating terrain than that in the Keping district during the Early Cambrian.Correlated with distribution of extant algae,it could be concluded that the difference in tectonic activity,water depth,and paleo-terrian may be the major cause for the difference in hydrocarbon generating organism assemblages between the Xishanbulake Formation in the Southern Yaerdangshan section and the Yuertus Formation the Dongergou section.

Key words: hydrocarbon generating organism assemblage, source rock, Yuertusi Formation, Xishanbulake Formation, Lower Cambrian, Tarim Basin

中图分类号:

TE122.1

胡广,刘文汇,腾格尔,等. 塔里木盆地下寒武统泥质烃源岩成烃生物组合的构造-沉积环境控制因素[J]. 石油与天然气地质, 2014, 35(5): 685-695. doi: 10.11743/ogg20140514 Hu Guang,Liu Wenhui,Tengger,et al. Tectonic-sedimentary constrains for hydrocarbon generating organism assemblage in the Lower Cambrian argillaceous source rocks, Tarim Basin[J]. Oil & Gas Geology, 2014, 35(5): 685-695. doi: 10.11743/ogg20140514

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塔里木盆地下寒武统泥质烃源岩成烃生物组合的构造-沉积环境控制因素

Tectonic-sedimentary constrains for hydrocarbon generating organism assemblage in the Lower Cambrian argillaceous source rocks, Tarim Basin

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[2]	张艳秋, 陈红汉, 王燮培, 王彭, 苏丹梅, 谢舟. 塔里木盆地富满油田走滑断裂带通源性评价[J]. 石油与天然气地质, 2024, 45(3): 787-800.
[3]	丁文龙, 李云涛, 韩俊, 黄诚, 王来源, 孟庆修. 碳酸盐岩储层高精度构造应力场模拟与裂缝多参数分布预测方法及其应用[J]. 石油与天然气地质, 2024, 45(3): 827-851.
[4]	曹自成, 云露, 漆立新, 李海英, 韩俊, 耿锋, 林波, 陈菁萍, 黄诚, 毛庆言. 塔里木盆地顺北地区顺北84X井超千米含油气重大发现及其意义[J]. 石油与天然气地质, 2024, 45(2): 341-356.
[5]	杨德彬, 鲁新便, 鲍典, 曹飞, 汪彦, 王明, 谢润成. 塔里木盆地北部奥陶系海相碳酸盐岩断溶体油藏成因类型及特征再认识[J]. 石油与天然气地质, 2024, 45(2): 357-366.
[6]	张长建, 杨德彬, 蒋林, 姜应兵, 昌琪, 马雪健. 塔里木盆地塔河北部“过溶蚀残留型”断溶体发育特征及其成因[J]. 石油与天然气地质, 2024, 45(2): 367-383.
[7]	万俊雨, 朱建辉, 姚素平, 张毅, 李春堂, 张威, 姜海健, 王杰. 鄂尔多斯盆地中、东部奥陶系马家沟组成烃生物及烃源岩地球生物学评价[J]. 石油与天然气地质, 2024, 45(2): 393-405.
[8]	江同文, 邓兴梁, 曹鹏, 常少英. 塔里木盆地富满断控破碎体油藏储集类型特征与注水替油效果[J]. 石油与天然气地质, 2024, 45(2): 542-552.
[9]	牛月萌, 韩俊, 余一欣, 黄诚, 林波, 杨帆, 余浪, 陈俊宇. 塔里木盆地顺北西部地区火成岩侵入体发育特征及其与断裂耦合关系[J]. 石油与天然气地质, 2024, 45(1): 231-242.
[10]	侯读杰, 吴克强, 尤丽, 张自鸣, 李雅君, 熊小峰, 徐敏, 严夏泽, 陈威合, 程熊. 琼东南盆地陆源海相烃源岩有机质富集机理[J]. 石油与天然气地质, 2024, 45(1): 31-43.
[11]	张三, 金强, 史今雄, 胡明毅, 段梦悦, 李永强, 张旭栋, 程付启. 塔北地区奥陶系地下河溶洞充填规律与储集性能[J]. 石油与天然气地质, 2023, 44(6): 1582-1594.
[12]	罗情勇, 钟宁宁, 李美俊, 吴进, Khan Imran, 张烨, 陈清, 叶祥忠, 李文浩, 纪文明, 刘安吉, 郝婧玥, 姚立朋, 吴嘉. 前寒武纪—早古生代沉积岩显微组分分类、成因及演化[J]. 石油与天然气地质, 2023, 44(5): 1084-1101.
[13]	吴进, 罗情勇, 钟宁宁, 方子龙, 段金材, 张无忌, 崔雅鑫. 华北北部中元古界下马岭组页岩有机岩石学研究[J]. 石油与天然气地质, 2023, 44(5): 1218-1230.
[14]	康志江, 张冬梅, 张振坤, 王睿奇, 姜文斌, 刘坤岩. 深层缝洞型油藏井间连通路径智能预测技术[J]. 石油与天然气地质, 2023, 44(5): 1290-1299.
[15]	胡伟, 徐婷, 杨阳, 伦增珉, 李宗宇, 康志江, 赵瑞明, 梅胜文. 塔里木盆地超深油气藏流体相行为变化特征[J]. 石油与天然气地质, 2023, 44(4): 1044-1053.