[1]张敏强,钟志洪,夏斌.2004.莺歌海盆地泥-流体底辟构造成因机制与天然气运聚.大地构造与成矿学,28(2):118-125.
 ZHANG Minqiang,ZHONG Zhihong,XIA Bin.2004.GENETIC MECHANISMS OF MUDFLUID DIAPIR IN YINGGEHAI BASIN AND HYDROCARBON ACCUMULATION.Geotectonica et Metallogenia,28(2):118-125.
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莺歌海盆地泥-流体底辟构造成因机制与天然气运聚
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2004年28卷02期
页码:
118-125
栏目:
出版日期:
2004-05-25

文章信息/Info

Title:
GENETIC MECHANISMS OF MUDFLUID DIAPIR IN YINGGEHAI BASIN AND HYDROCARBON ACCUMULATION
作者:
张敏强1钟志洪1夏斌1李绪宣1孙珍2王良书3王振峰4
1. 中国科学院广州地球化学研究所, 广东 广州 510640; 2. 中国科学院南海海洋研究所, 广东 广州510301; 3. 南京大学地球科学系,江苏 南京 210093; 4. 中海油湛江分公司,广东 湛江 524057
Author(s):
ZHANG Minqiang1 ZHONG Zhihong1 XIA Bin1 LI Xuxuan1 SUN Zhen2WANG Liangshu3 and Wang Zhenfeng4
1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, GD 510301, China; 3. The Department of Earth Sciences, Nanjing University, Nanjing, JS 210093, China; 4. Nanhai West Corporation, CNOOC, Zhanjiang, GD 524057, China
关键词:
莺歌海盆地泥-流体底辟不均衡压实热作用幕式充注
Keywords:
Yinggehai basin mudfluid diapir disequilibrium compaction thermal evolution episodic injection
分类号:
P315.2; P618.13
文献标志码:
A
摘要:
莺歌海盆地的泥-流体底辟构造发育演化是区域构造应力场变化和超压体系形成演化的结果。与盆地构造类型密切相关的不均衡压实和热作用引起盆地超压体系的发育,而区域构造应力场变化则导致盆地中中新世以泥底辟作用为主,晚中新世—第四纪以流体底辟作用为主,其中,早期泥底辟阶段形成的构造形态对晚期流体底辟作用有显著的控制作用。在莺歌海组浅层底辟圈闭中,圈闭形成期与中新统气源岩生烃过程的匹配是造成含不同天然气组分的流体发生幕式充注的主要原因。
Abstract:
The evolution of mudfluid diapir in Yinggehai Basin is the result of regional stress field variation and overpressure system formation and evolution. Development of the overpressure system is caused by disequilibrium compaction and thermal evolution that are intimately related to the structural styles of the basin. Variation of the regional stress field resulted in the muddiapirism in midMiocene and the fluid diapirism in late Miocene to Quaternary. The structures formed during the early muddiapirism stage obviously controlled the later stage fluid diapirism. For the shallow traps in Yinggehai Formation, the main reason for episodic injection of fluid with different gas components is the matching of trap formation and hydrocarbon generation in Miocene.

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备注/Memo

备注/Memo:
收稿日期:20030918;改回日期:20031218基金项目:中国科学院知识创新项目(编号KZCX2SW11702)的部分成果.作者简介:张敏强(1958),男,博士生,高级地质师,主要从事石油地质综合研究.
更新日期/Last Update: 2004-05-15