石油与天然气地质 ›› 1984, Vol. 5 ›› Issue (4): 362-371.doi: 10.11743/ogg19840407

• 论文 • 上一篇    下一篇

广西百色盆地石油地质概述

蔡舜天, 郭亦秋   

  1. 广西石油勘探开发指挥部
  • 收稿日期:1984-04-16 出版日期:1984-12-25 发布日期:2012-01-16

AN OUTLINE OF PETROLEUM GEOLOGY OF BAISE BASIN

Cai Shuntian, Guo Yiqiu   

  1. Headquarters of Petroleum Prospecting and Exploration, Guangxi Province
  • Received:1984-04-16 Online:1984-12-25 Published:2012-01-16

摘要:

百色盆地地处广西西部,东起思林,西至百色,长109公里,宽2—9公里,面积830平方公里。盆地的石油地质工作已有几十年的历史,在七十年代进行了大规模的综合勘探,结果在田东凹陷的北部找到了油气富集区,为建设广西第一个石油基地创造了条件。

Abstract:

Baise Basin,located in the western part of Guangxi Province,is a narrow Tertiary sedimentary basin striking NW and occupying an area of 830km2.This basin is the biggest one among the five Tertiary basins in Guangxi Province and has a history over 20 years in petroleum prospecting.The Tertiary sediments in this basin are of 2,700-3,400m thick.Among other things,the late Eocene Nadu Formation (E3n) and the Oligocene Baigang Formation (E3b) are both source rocks and reservoir rocks.In addition,lime-stones of the middle Triassic Lanmu Formation (T2l),which constitutes the basement of the basin,also serve as reservoir rocks.Source rocks of Nadu For-mation is as thick as 700m.Organic matters in the rocks are primarily sapropel or intermediate types.Geothermal gradient observed in this basin is 3.4℃/100m.The thresholds of oil generation are respectively 1,200m (64℃) and 1,400m(71℃).The basin could be divided into three depressions and two uplifts,i.e.Tiandong,Baise and Tianyang depressions and Nabai and Sitang uplifts.Tiandong is the biggest depression among the three and has been highly ex-plorated.Till now,8 oil and gas pools discovered are all distributed along this depression and the neibouring Nabai uplift.The step-faulted zone in north of the depression is oil and gas enrich zone.Oil pools in this basin are in various small traps,such as anticlinal trap,fault block trap,lithological trap or even more complicated trap.The buried depth is 22.6-1,935m.Crude oil is low-sulphur paraffin-base,and is charac-terized almost by primary or oxidized type.Some oil traps are capped with gas.The formation waters are NaHCO3 type.