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Large‐scale Tazhong Ordovician Reef‐flat Oil‐Gas Field in the Tarim Basin of China
Author(s) -
ZHOU Xinyuan,
WANG Zhaoming,
YANG Haijun,
ZHANG Lijuan,
HAN Jianfa,
WANG Zhenyu
Publication year - 2009
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/j.1755-6724.2009.00020.x
Subject(s) - geology , reef , ordovician , hermatypic coral , karst , lithology , tarim basin , natural gas field , geomorphology , geochemistry , paleontology , oceanography , natural gas , chemistry , organic chemistry
The Tazhong reef‐flat oil‐gas field is the first large‐scale Ordovician organic reef type oil‐gas field found in China. Its organic reefs were developed in the early Late Ordovician Lianglitag Formation, and are the first large reefs of the coral‐stromatoporoid hermatypic community found in China. The organic reefs and platform‐margin grain banks constitute a reef‐flat complex, mainly consisting of biolithites and grainstones. The biolithites can be classified into the framestone, bafflestone, bindstone etc. The main body of the complex lies around the wells from Tazhong‐24 to Tazhong‐82, trending northwest, with the thickness from 100 to 300 m, length about 220 km and width 5–10 km. It is a reef‐flat lithologic hydrocarbon reservoir, with a very complex hydrocarbon distribution: being a gas condensate reservoir as a whole with local oil reservoirs. The hydrocarbon distribution is controlled by the reef complex, generally located in the upper 100–200 m part of the complex, and largely in a banded shape along the complex. On the profile, the reservoir shows a stratified feature, with an altitude difference of almost 2200 m from southeast to northwest. The petroleum accumulation is controlled by karst reservoir beds and the northeast strike‐slip fault belt. The total geologic reserves had reached 297.667 Mt by 2007.