Episodic fluid movements in superimposed basin: Combined evidence from outcrop and fluid inclusions of the Majiang ancient oil reservoir, Guizhou Province

被引:7
|
作者
Xiang CaiFu [1 ,2 ]
Tang LiangJie [1 ,2 ]
Li RuFeng [1 ,2 ]
Pang XiongQi [1 ,2 ]
机构
[1] China Univ Petr, Basin & Reservoir Res Ctr, Beijing 102249, Peoples R China
[2] China Univ Petr, State Key Lab Petr Resource & Prospecting, Beijing 102249, Peoples R China
来源
SCIENCE IN CHINA SERIES D-EARTH SCIENCES | 2008年 / 51卷 / Suppl 2期
基金
中国国家自然科学基金;
关键词
Majiang ancient oil reservoir; episodic fluid flow; marine carbonate rocks; superimposed basin;
D O I
10.1007/s11430-008-6028-3
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Combined evidence from the outcrop and the fluid inclusion assemblage (FIA) analysis indicates that there exist two episodes of fluid flow controlled by the tectonic activity. The first episode was recorded mainly in the reservoir rock of the Honghuayuan Formation, representing the fluid flow of hydrocarbon charging. The second episode occurred mainly along the fault systems, representing the fluid movement when the ancient oil reservoir was destroyed. The host mineral morphology, homogeneous temperature, and salinity of the FIAs record an episodic fluid movement. Characters of high homogenous temperature, low salinity and a quick temperature variation of the first episode fluid flow may indicate an early-stage fluid eruption, and correspondingly, fine-grained calcite was formed. Temperature of the erupted fluid tended to decrease during its mixing with the upper formation fluid and finally had the same temperature as the upper formation. From then on, the temperature was rather steady and favored the growth of the coarse calcite. Due to this character of the temperature variation of the episodic fluid flow, we can use the homogenous temperature of the FIA of the coarse calcite to date the formation and the destruction time of the Majiang ancient oil reservoir. Episodic fluid flow was known for its inhomogeneous trapping, which resulted in the failure of dating according to the burial history. But taking a close look at its temperature variation, we think that the latest stage of fluid flow, characterized by steady state temperature and grow of the coarser crystals, can be used for dating. It will be of great value if this method is proved to be effective. The formation and the destruction time of the Majiang ancient oil reservoir were dated to be in the Indosinian Period and the late Yanshan-early Hymalayan Period respectively. This conclusion is in great discrepancy with the common accepted idea that the Majiang ancient oil reservoir was formed and destroyed during the Caledonian tectonic movement. Even so, this paper further discussed its reliability from the view of the source rock evolution and also the local tectonic evolution.
引用
收藏
页码:78 / 87
页数:10
相关论文
共 50 条
  • [41] Discussion of migration and precipitation mechanics in Muluo REE deposit Mianning county, west Sichuan province: Evidence from fluid inclusions in bastnaesite
    Xie YuLing
    Tian ShiHong
    Hou ZengQian
    Chen Wei
    Yin ShuPing
    Gao Sheng
    ACTA PETROLOGICA SINICA, 2008, 24 (03) : 555 - 561
  • [42] Genesis of the Nanyangtian scheelite deposit in southeastern Yunnan Province,China: evidence from mineral chemistry,fluid inclusions,and C–O isotopes
    Qianru Cai
    Yongfeng Yan
    Guangshu Yang
    Fuju Jia
    Chao Li
    ActaGeochimica, 2018, 37 (04) : 614 - 631
  • [43] Genesis of the Nanyangtian scheelite deposit in southeastern Yunnan Province, China: evidence from mineral chemistry, fluid inclusions, and C–O isotopes
    Cai Q.
    Yan Y.
    Yang G.
    Jia F.
    Li C.
    Yan, Yongfeng (yyf701018@vip.sina.com), 2018, Science Press (37): : 614 - 631
  • [44] Genesis of Chambishi Copper Deposit in Copperbelt Province of Zambia: Evidence from Fluid Inclusions and H-O-S Isotope Geochemisty
    Hu Q.
    Feng Z.
    Mo J.
    Fang K.
    Liu J.
    Cai Y.
    Deng G.
    Huang X.
    Bai L.
    Qin P.
    Diqiu Kexue - Zhongguo Dizhi Daxue Xuebao/Earth Science - Journal of China University of Geosciences, 2021, 46 (05): : 1554 - 1568
  • [45] Genesis of the Nanyangtian scheelite deposit in southeastern Yunnan Province,China: evidence from mineral chemistry,fluid inclusions,and C–O isotopes
    Qianru Cai
    Yongfeng Yan
    Guangshu Yang
    Fuju Jia
    Chao Li
    Acta Geochimica, 2018, (04) : 614 - 631
  • [46] Characteristics of Fluid Inclusions and Hydrocarbon Accumulation Stages of Carbonate Rock Reservoir: A Case Study from the Majiagou Formation Ordovician, Central and Eastern Ordos Basin
    Liu, Yanzhao
    Ren, Zhanli
    Qi, Kai
    Yan, Xinyun
    Xiong, Beile
    Liu, Jian
    Ren, Junfeng
    Xing, Guangyuan
    Jia, Mingxing
    Yao, Juwen
    Tian, Hongwei
    MINERALS, 2025, 15 (02)
  • [47] Impact of Overpressure on the Preservation of Liquid Petroleum: Evidence from Fluid Inclusions in the Deep Reservoirs of the Tazhong Area, Tarim Basin, Western China
    Su, Peng
    Zhang, Jianyong
    Zhou, Zhenzhu
    Chen, Xiaolan
    Zhang, Chunrong
    ENERGIES, 2024, 17 (19)
  • [48] Multistage petroleum charges in the Silurian of Tazhong north slope of the Tarim basin, northwest China: evidence from fluid inclusions and organic geochemistry
    Pan LiYin
    Ni Pei
    Ou GuangXi
    Li LinQiang
    ACTA PETROLOGICA SINICA, 2007, 23 (01) : 131 - 136
  • [49] Feature of ore-forming fluid: Evidence from fluid inclusion, REE and carbon-oxygen isotope geochemistry of calcite from Huangjiawan Mo-Ni polymetallic ore deposit, Zunyi, Guizhou Province
    Feng CaiXia
    Chi GuoXiang
    Hu RuiZhong
    Liu Shen
    Liu JiaJun
    Luo TaiYi
    Qi YouQiang
    ACTA PETROLOGICA SINICA, 2011, 27 (12) : 3763 - 3776
  • [50] LATE THERMAL EVENTS IN THE MESOZOIC BASQUE BASIN - EVIDENCE FROM SECONDARY FLUID INCLUSIONS IN MISSISSIPPI-VALLEY TYPE FLUORITE OCCURRENCES
    HERRERO, JM
    PEREZALVAREZ, M
    TOURAY, JC
    VELASCO, F
    BULLETIN DE MINERALOGIE, 1988, 111 (3-4): : 413 - 420