松辽盆地营城组火山机构地层结构定量模型

doi:10.7623/syxb201204002

石油学报 ›› 2012, Vol. 33 ›› Issue (4): 541-550.DOI: 10.7623/syxb201204002

松辽盆地营城组火山机构地层结构定量模型

唐华风 1　白　冰 1　边伟华 1　王力圆 2　孙海波 1

1　吉林大学地球科学学院　吉林长春　130061；　2　重庆地质矿产研究院　重庆　400042

收稿日期:2012-01-31 修回日期:2012-05-07 出版日期:2012-07-25 发布日期:2012-08-01
通讯作者: 唐华风
作者简介:唐华风，男，1979年6月生，2001年获吉林大学学士学位，2007年获吉林大学博士学位，现为吉林大学地球科学学院副教授，主要从事火山岩储层地质-地球物理研究。
基金资助:
国家自然科学青年基金项目（No.41002038）、国家重点基础研究发展计划（973）项目(2009CB219303)和吉林大学科学前沿与交叉学科创新项目(200903027)资助。

Quantitative models of strata texture within volcanic edifices of Yingcheng Formation in Songliao Basin, NE China

TANG Huafeng 1　BAI Bing 1　BIAN Weihua 1　WANG Liyuan 2　SUN Haibo 1

Received:2012-01-31 Revised:2012-05-07 Online:2012-07-25 Published:2012-08-01

摘要/Abstract

摘要：

松辽盆地营城组火山岩地层主要由火山机构侧向迁移和垂向叠置而形成。目前对火山机构的内部结构认识还不清晰，制约了火山岩勘探开发进程。通过对典型酸性熔岩、酸性复合、酸性碎屑岩和中基性熔岩火山机构的综合解剖，建立其地层结构模型。酸性火山机构中多数为似层状结构，中基性火山机构中除发育似层状结构外，还常见层状结构。具有似层状结构的酸性火山机构的岩层倾角要大于具有层状结构的中基性熔岩火山机构；现今岩层倾角可为正态分布，也可呈现出偏正态或双峰态。火山岩地层结构与火山机构类型、喷发古环境（同生断层和古斜坡）密切相关；后期的挤压和掀斜作用对岩层产状变化起到显著的改造作用；后期单期次、断距小的正断层或逆断层的改造，对岩层产状的变化影响较小。此研究为火山岩地层结构内部精细解剖提供了理论依据。

关键词: 松辽盆地, 营城组, 火山地层, 似层状结构, 控制因素

Abstract:

The volcanostratigraphy of Yingcheng Formation was built up by volcanic edifices which migrated in lateral direction and overlapped in vertical succession. In present, internal structures of volcanic edifices are not clear. So development process of volcanic gas pools in Songliao Basin was decelerated. The models of strata texture within volcanic edifices were created by integrated analysis of acid lava, acid compound, and acid pyroclastic volcanic edifices as well as intermediate-basic lava ones. The strata texture of mostly acid volcanic edifices is pseudostratified texture. The intermediate-basic lava volcanic edifices has stratified texture besides the pseudostratified texture. The dip angle of acid volcanic edifices (with the pseudostratified texture) is bigger than that of the intermediate-basic volcanic edifices (with the stratified texture). The dip angles show normal distribution, skewed normal distribution or bimodal shape. The primary stratified occurrence of volcanic rocks is controlled by types of volcanic edifices, eruptive paleogeomorphology (such as contemporaneous fault and paleoslope), and reformed by later compressional and tilting activities. Purly later low relief normal faults or reverse faults can impact the occurrence slightly. This study offers a theoretical basis for meticulous depiction of internal structure of volcanostratigraphy.

Key words: Songliao Basin, Yingcheng Formation, volcanostratigraphy, pseudostratified texture, controlling factors

唐华风　白　冰　边伟华　王力圆　孙海波. 松辽盆地营城组火山机构地层结构定量模型[J]. 石油学报, 2012, 33(4): 541-550.

TANG Huafeng　BAI Bing　BIAN Weihua　WANG Liyuan　SUN Haibo. Quantitative models of strata texture within volcanic edifices of Yingcheng Formation in Songliao Basin, NE China[J]. Editorial office of ACTA PETROLEI SINICA, 2012, 33(4): 541-550.

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松辽盆地营城组火山机构地层结构定量模型

Quantitative models of strata texture within volcanic edifices of Yingcheng Formation in Songliao Basin, NE China

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