THE ORDOVICIAN CARBONIC RESERVOIR CHARACTERISTICS ANDMINERALIZATION IN YINGMAILI LOW HEAVE OF TARIM BASIN
Received date: 2005-05-18
Revised date: 2005-07-26
Online published: 2005-10-20
The yingmail low heave carbonic buried hill includes gray, dark-gray, offwhiteand dust-colour biologic, sandstonic, strumae, mud carbonate And dolomite. It isseparated eight lithology sects from up to down:Mud carbonate, gray matter mud,strumaed carbnote, biologic carbnote, flint carbnote, mud and biologic carbonate, dolomitic carbnote, carbnotic dolonate.It is separated five mineralization types:exposure bank, harst, deep buried dolomite, paleo-carbonate buried hill, tectonic-rimose and so on. In the long geologic evolvement,it lived seawater mineralization condition, mixed water mineralization condition, vaporized seawater mineralization condition, forepart fresh water mineralization condition, buried mineralization condition.
LIU Yu-kui, ZHENG Duo-ming,WANG Jian-ning,MIN Lei,WU Jian-guo,FENG You-wen . THE ORDOVICIAN CARBONIC RESERVOIR CHARACTERISTICS ANDMINERALIZATION IN YINGMAILI LOW HEAVE OF TARIM BASIN[J]. Natural Gas Geoscience, 2005 , 16(5) : 587 -591 . DOI: 10.11764/j.issn.1672-1926.2005.05.587
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