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准南地区下二叠统火山岩-沉积岩互层叠置发育模式
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  • 英文篇名:Developmental patterns of interbedded volcanic and sedimentary rocks in the Lower Permian of Zhunnan area
  • 作者:孙莹
  • 英文作者:SUN Ying;Exploration and Development Research Institute,Shengli Oilfield Company,SINOPEC;
  • 关键词:下二叠统 ; 火山岩-沉积岩 ; 互层叠置 ; 发育模式 ; 准南地区
  • 英文关键词:Lower Permian;;volcanic-sedimentary rocks;;interbed;;developmental pattern;;Zhunnan area
  • 中文刊名:YQCS
  • 英文刊名:Petroleum Geology and Recovery Efficiency
  • 机构:中国石化胜利油田分公司勘探开发研究院;
  • 出版日期:2018-06-06 10:23
  • 出版单位:油气地质与采收率
  • 年:2018
  • 期:v.25;No.133
  • 基金:中国石化科技攻关项目“准噶尔盆地大中型油气田分布规律与目标评价”(P17001-7)
  • 语种:中文;
  • 页:YQCS201804005
  • 页数:6
  • CN:04
  • ISSN:37-1359/TE
  • 分类号:32-36+64
摘要
通过野外露头观测与样品采集,对准南地区下二叠统火山岩-沉积岩互层叠置发育特征和发育模式开展火山岩相学、样品测试和室内综合分析等研究。结果表明:研究区火山岩以基性火山岩(玄武岩)和酸性火山岩(英安斑岩或流纹岩)伴生出现为主要特征,具有双峰式火山岩的岩石组合特征。沉积岩以砾岩、砂砾岩为主,砾石成分主要为火山岩和火山碎屑岩,成分成熟度和结构成熟度均较低。火山岩-沉积岩互层叠置地层序列以玄武岩、英安斑岩与火山角砾岩或砂泥岩互层产出为特征,划分为火山爆发相、次火山岩相、火山喷溢相、冲积扇扇根亚相、冲积扇扇中亚相和冲积扇扇缘亚相6种岩相类型以及中性旋回、中-酸性旋回、沉积旋回和基性火山-沉积旋回4个旋回。在大陆裂谷的背景下,软流圈地幔上涌形成的玄武质岩浆与其底侵下地壳物质发生熔融形成的酸性岩浆混合,形成流纹岩或流纹斑岩、玄武岩,与火山活动间歇期形成的沉积岩互层叠置。
        Based on outcrop observation and sample collection in the field,the study of developmental patterns and characteristics of interbedded volcanic and sedimentary rocks in the Lower Permian of Zhunnan area was carried out through volcanic petrographic analysis,sample test and indoor comprehensive analysis. The result shows that the volcanic rocks in this area are mainly composed of basic volcanic rocks(basalt)and its associated acidic volcano rocks(dacite porphyry or rhyolite),which would be present as bimodal volcanic rock combination characteristics. Conglomerates and glutenite are mainly developed in the sedimentary rocks. The main components of the gravel are volcanic rocks and pyroclastic rocks,and their composition maturity and structural maturity are relatively low. The sequence of interbedded volcanic and sedimentary rock strata is characterized by alternation of basalt,dacite porphyry and volcanic breccia or sand and mudstone. Six types of lithofacies can be divided as volcanic eruption facies,subvolcanic facies,volcanic effusive facies,alluvial fan fan-root subfacies,alluvial fan fan-middle subfacies and alluvial fan margin subfacies. Four cycles can be divided as neutral cycle,neutral-acid cycle,sedimentary cycle and basic volcanic sedimentary cycle. Under the structural background of continental rift,the basaltic magma formed by the upwelling asthenosphere mantle is melted with the undercut crustal material to become mixed acidic magma,and thus the rhyolite,rhyolite porphyry and basalt were formed,interbedded with the sedimentary rocks formed during the intermittence period after the volcanic activity.
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