席勤,余和中,顾乔元,钱玲,李新生,李毓丰
XI Qin,YU Hezhong,GU Qiaoyuan,QIAN Ling,LI Xinsheng,LI Yufeng

• 1:中国石油塔里木油田分公司
• 2:中国石油杭州地质研究院

摘要(Abstract)：

通过区域构造、主要烃源岩分布及地球化学特征等研究,明确了阿瓦提凹陷发育的主力烃源岩。结果表明:阿瓦提凹陷发育有中—下寒武统、中—上奥陶统和石炭系—二叠系等3套烃源岩;中—下寒武统烃源岩在加里东晚期进入生油门限,处于低熟阶段,海西早期处于成熟高峰阶段,海西晚期处于高峰—高熟阶段,燕山期处于高熟—过熟峰期,喜马拉雅晚期处于过熟阶段;中—上奥陶统烃源岩主要分布于阿瓦提凹陷的西北部,加里东晚期—海西早期处于未成熟阶段,海西晚期处于低熟—成熟阶段,燕山期处于成熟高峰期,喜马拉雅晚期处于高熟—过熟阶段。
With the help of the studies on the regional tectonics,main hydrocarbon source rock distribution,geochemical characteristics and so on,the key hydrocarbon source rocks developed in Awati Sag are made clear.The achievements show that there are three sets of the source rocks developed in the sag:Middle- Lower Cambrian series,Middle- Upper Ordovician series and Carboniferous-Permian system:the rocks in the former entered into the generation threshold-low mature stage in the later period of Caledonian orogeny,into the peak mature stage in the early period of Hercynian orogeny,into the peak-high mature stages in the later period of Hercynian orogeny,into the high-over mature stages in the period of Yanshan orogeny,into the over mature stage in the later period of Himalayan;the middle is mainly distributed in Northwest Awati Sag,the immature stage is distributed in the later period of Caledonian orogeny and early period of Hercynian orogeny,the low-over mature stages are in the later period of Hercynian orogeny,the peak mature stage is in the period of Yanshan orogeny,the high-over mature stages are in the later period of Himalayan orogeny.

关键词(KeyWords)： 塔里木盆地;阿瓦提凹陷;地球化学;寒武系;烃源岩
Tarim Basin;Awati Sag;geochemistry;Cambrian;source rock

Abstract:

Keywords:

基金项目(Foundation): 国家重点基础研究发展计划“973”项目“中国西部叠合盆地油气富集规律与勘探潜力预测”(2011CB201106)

作者(Author): 席勤,余和中,顾乔元,钱玲,李新生,李毓丰
XI Qin,YU Hezhong,GU Qiaoyuan,QIAN Ling,LI Xinsheng,LI Yufeng

参考文献(References)：

• [1]张水昌,梁狄刚,张宝民,等.塔里木盆地海相油气的生成[M].北京:石油工业出版社,2004:101-102,376
• [2]李君文,陈洪德,田景春,等.沉积有机相的研究现状及其应用[J].沉积与特提斯地质,2004,24(2):96-100
• [3]王飞宇,杜治利,张宝民,等.柯坪剖面中上奥陶统萨尔干组黑色页岩地球化学特征[J].新疆石油地质,2008,29(6):687-689
• [4]顾忆,赵永强,贾存善,等.塔里木盆地阿瓦提坳陷油气潜力分析[J].石油实验地质,2012,34(3):257-266
• [5]余和中,蔡希源,韩守华,等.松辽盆地石炭—二叠系烃源岩研究[J].沉积与特提斯地质,2003,23(2):62-66
• [6]卢玉红,钱玲,张海祖,等.塔里木阿瓦提凹陷乌鲁桥油苗地化特征及来源[J].海相油气地质,2008,13(2):45-51
• [7]张艳,王璞珺,陈文礼,等.有效烃源岩的识别与应用:以塔里木盆地为例[J].大庆石油地质与开发,2006,25(6):9-12
• [8]雷涛,周文,邓虎成,等.塔中地区海相烃源岩测井评价[J].大庆石油地质与开发,2011,30(2):170-174
• [9]王秋玲,贾望鲁,彭平安,等.柯坪隆起阿克苏油苗地球化学特征及其成因研究[J].地球化学,2012,4l(1):45-54
• [10]包建平,朱翠山,黄光辉,等.甲基菲比值与有机质成熟度演化的关系[J].江汉石油学院学报,1992,14(4):8-13
• [11]张水昌,梁狄刚,张宝民,等.分子化石与塔里木盆地油源对比[J].科学通报,2002,47(增1):16-23
• [12]王兴光,苗洪波,李建臣,等.原油与其烃源岩中甾萜类化合物指标的差异[J].大庆石油地质与开发,2008,27(1):18-21
• [13]曾花森,蔡郁文,霍秋立,等.烃源岩中有效有机质的类型评价及意义[J].大庆石油地质与开发,2013,32(3):8-14
• [14]刘晓艳,黄薇.有机相的综合评价指标:OFI及其应用[J].大庆石油地质与开发,1997,16(4):16-19