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引用本文:刘特民,刘炳温,陈国栋,吴正永. ���̽���ع����ݻ�����������������[J]. 天然气工业, 2001, 21(1): 18-22,23
作者姓名:刘特民  刘炳温  陈国栋  吴正永
作者单位:???????????????
摘    要:综合分析大量实际资料、MT和地震最新成果之后认为:南盘江盆地基底位地加里里东期扬子板块被动大陆边缘两侧。海西期出现板内拉张裂陷,形成台盆格局,生物礁灰岩发育。印支期出现早期前陆盆地海相复理只,由于早印支运动使T2砂泥岩揉褶成山,晚期前陆盆地夭折,经印支一燕山褶断运动和喜山期的改造后,最终出现田林T2砂泥岩覆盖区,即田林油气保存区,成为油气勘探的主要地区。该区具有受力相对较弱,中深层海西构造层背斜大而完整,且有P2-P1m丘 岩发育,D1-2gf丘台礁灰岩从MT资料发现多处,主要勘探目标明确。但该区在按部颁标准进行构造单元划分、区带评价、优选圈闭和钻探井位时,明显地感到对本区不合适。因而提出用油气保存区、保存分区和保存单元三级划分取代原构造单元三级划分,并提出划分依据、评价原则和初步划分表,阐述保存区可供勘探的主要目标和特点,在盆地整体评价较差的情况下也能够优选出保存单元进行勘探。

关 键 词:南盘江 裂谷盆地 前陆盆地 构造演化 油气藏保存条件
修稿时间:2000-07-18

Tectonic Evolution and Hydrocarbon Preservation Region Division in Nanpanjiang Basin
Liu Temin,Liu Bingwen,Chen Guodong and Wu Zhengyong. Tectonic Evolution and Hydrocarbon Preservation Region Division in Nanpanjiang Basin[J]. Natural Gas Industry, 2001, 21(1): 18-22,23
Authors:Liu Temin  Liu Bingwen  Chen Guodong  Wu Zhengyong
Affiliation:Guizhou Research Institute of Petroleum Geology
Abstract:??After having comprehensively analyzed a great deal of practical data and the newest MT and seismic achievements,it is considered that the basement of Nanpanjiang Basin was located in the both sides of the passive continental margin of Caledonian Yangzi Plate;an introplate tension taphrogenic depression occurred in Hercynian,forming a platformal basin framework with grown biohermal limestomes;the marine flysch deposition of early foreland basin appeared in Indosinian;owing to early Indosinian movement the sand mudstones(T2)were folded into mountains,which made the late foreland basin be withered away;and reformed by Indosinian Yanshanian orogeny and Himalayan orogeny,the Tianlin sand mudstone(T2)covering region,i.e.the Tianlin hydrocarbon preservation region,appeared at last,becoming the major area of oil and gas exploration.This region is of the properties as being relatively weaker forced,large and full medium deep Hercynian structural layer anticlines and grown mound table reef limestones(P2??P1m),etc.In the region,the principal exploration target is clear,because the mound table reef limestones(D12gf)were found at several places by MT data.However,it is unsuitable to carry out structural element division,regional evaluation and the optimization of trap and well location according to the ministerial standard.So a new 3 class division,i.e.hydrocarbon preservation region,preservation subregion and preservation unit is proposed to take the place of the former 3 class structural element division and the division bases,evaluation principle and primary dividing table are put forward.On the basis of this,the major exploration targets in the preservation region and their properties are analyzed,so some preservation units can be also optimized for exploration under the circumstances of a lower basin evaluation as a whole
Keywords:Nanpanjiang River  Rift Basin  Foreland Basin  Reef  Limestone  Reservoir preservation condition  Preservation unit  
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