中国石油勘探 ›› 2019, Vol. 24 ›› Issue (6): 739-749.DOI: 10.3969/j.issn.1672-7703.2019.06.006

• 石油地质 • 上一篇    下一篇

准噶尔盆地滴南凸起石炭系古火山机构地震特征及有利区预测

代春萌1 ,曾庆才1 ,李波2 ,徐淑娟1 ,李璇1 ,杨亚迪1   

  1. 1 中国石油勘探开发研究院;2 中国石油新疆油田公司
  • 出版日期:2019-11-15 发布日期:2019-11-15
  • 基金资助:
    国家科技重大专项“大型油气田及煤层气开发”(2016ZX05051-004)。

Seismic characteristics of Carboniferous ancient volcanic edifices and prediction of favorable zones in the Dinan bulge of the Junggar Basin

Dai Chunmeng1, Zeng Qingcai1, Li Bo2, Xu Shujuan1, Li Xuan1, Yang Yadi1   

  1. 1 PetroChina Research Institute of Petroleum Exploration & Development; 2 PetroChina Xinjiang Oilfield Company
  • Online:2019-11-15 Published:2019-11-15
  • Supported by:
     

摘要: 准噶尔盆地滴南凸起石炭系古火山机构复杂,对气藏形成分布和勘探开发有重要影响。基于最新钻井、 测井及三维地震数据解释成果,开展滴南凸起石炭系古火山机构特征研究,分析古火山机构对气藏的控制作用。研究 认为:①根据火山机构形态和火山岩成分,滴南凸起石炭系古火山机构可划分为裂隙式熔岩火山机构、中心式单火山 口碎屑岩火山机构、中心式多火山口复合火山机构、裂隙式侵入火山机构4 种类型,受火山喷发—沉积旋回控制,早 石炭世以中心式单火山碎屑岩火山机构及裂隙式侵入火山机构为主,晚石炭世以裂隙式熔岩火山机构为主。②古火山 机构控制优质储层类型及分布,裂隙式熔岩火山机构发育玄武岩储层,中心式单火山口碎屑岩火山机构发育火山角砾 岩和英安岩储层,中心式多火山口复合火山机构发育火山角砾岩和玄武岩储层,裂隙式侵入火山机构发育花岗斑岩储 层。③受古火山机构控制发育火山内幕气藏、风化壳气藏、构造—岩性气藏3 种类型,有深大断裂沟通的古火山机构 为油气运移的有利指向。

 

关键词: 滴南凸起, 石炭系, 古火山机构, 火山岩储层, 气藏类型, 成藏模式

Abstract: The Carboniferous ancient volcanic edifices are complex, and have an important impact on the formation, distribution, exploration and development of the gas reservoirs in the Dinan bulge of the Junggar Basin. Based on the interpretation results of new drilling, logging and 3D seismic data, the characteristics of the Carboniferous ancient volcanic edifices and their control on the gas reservoirs were studied and analyzed in the Dinan bulge. The study gives the conclusions as follows: a. According to the morphology of the volcanic edifices and the composition of the volcanic rock, the Carboniferous ancient volcanic edifices can be divided into four types including fractured lava volcanic edifice, central single-crater clastic volcanic edifice, central multi-crater composite volcanic edifice and fractured intrusive volcanic edifice. Controlled by volcanic eruption and sedimentary cycles, the Early Carboniferous volcanic edifices are mainly central single-crater clastic volcanic edifices and fractured intrusive volcanic edifices, and the Late Carboniferous are dominated by fractured lava volcanic edifices. b. The ancient volcanic edifices control the type and distribution of high-quality reservoirs: the fractured lava volcanic edifices contain basaltic reservoirs, the central single-crater clastic volcanic edifices have breccia and dacite reservoirs, and the central multi-crater composite volcanic edifices have breccia and basalt reservoirs, and the fractured intrusive volcanic edifices provide granite porphyry reservoirs. c. Controlled by the ancient volcanic edifices, there are inside-volcano gas reservoirs, weathering crust gas reservoirs, and structural-lithologic gas reservoirs; and the ancient volcanic edifices connecting to deep and large faults are favorable targets for hydrocarbon migration.

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