山东省灵山岛下白垩统青山群火山地震软沉积物变形构造特征及成因机制<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2017.04.044

古地理学报 ›› 2017, Vol. 19 ›› Issue (4): 567-582. doi: 10.7605/gdlxb.2017.04.044

• 岩相古地理学及沉积学 • 下一篇

山东省灵山岛下白垩统青山群火山地震软沉积物变形构造特征及成因机制^*

周瑶琪^1,2, 周腾飞^1,2, 张振凯^1,2, 梁钊^1,2, 梁文栋³, 王安东⁴, 于姗姗⁵

1 中国石油大学(华东)地球科学与技术学院,山东青岛 266580;
2 中国石油大学(华东)地球化学与岩石圈动力学开放实验室,山东青岛 266580;
3 米兰比可卡大学地球与环境科学系, 米兰 20126, 意大利;
4 山东黄河三角洲国家级自然保护区管理局,山东东营 257091;
5 中海石油研究总院,北京 100027

收稿日期:2016-08-26 修回日期:2016-10-21 出版日期:2017-08-01 发布日期:2017-08-07
作者简介:周瑶琪,男,1963年生,中国石油大学(华东)地球科学与技术学院教授、博士生导师,主要从事地球化学、地球动力学及盆地沉积学的教学与科研工作。E-mail: zhouyq@upc.edu.cn。
基金资助:
*国家自然科学基金项目(编号: 41272123)和中央高校基本科研业务费专项资金项目(编号:15CX06011A)联合资助

Characteristics and formation mechanism of soft-sediment deformation structures related to volcanic earthquakes of the Lower Cretaceous Qingshan Group in Lingshan Island, Shandong Province

Zhou Yaoqi^1,2, Zhou Tengfei^1,2, Zhang Zhenkai^1,2, Liang Zhao^1,2, Liang Wendong³, Wang Andong⁴, Yu Shanshan⁵

1 School of Geosciences,China University of Petroleum(East China),Qingdao 266580,Shandong;
2 Laboratory of Geochemistry & Lithosphere Dynamics,China University of Petroleum(East China),Qingdao 266580,Shandong;
3 Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milano 20126, Italy;
4 Authority of Shandong Yellow River Delta National Nature Reserve,Dongying 257091,Shandong;
5 CNOOC Research Institute,Beijing 100027;

Received:2016-08-26 Revised:2016-10-21 Online:2017-08-01 Published:2017-08-07
About author:Zhou Yaoqi,born in 1963,is a professor and doctoral supervisor in China University of Petroleum(East China). He is mainly engaged in teaching and researches of geochemistry,geodynamics and basin sedimentology. E-mail: zhouyq@upc.edu.cn.
Supported by:
Co-funded by the National Natural Science Foundation of China(No.41272123) and the Fundamental Research Funds for the Central Universities (No.15CX06011A)

摘要/Abstract

摘要： 近年来,针对山东省灵山岛地区软沉积物变形构造的研究呈现热潮,但研究层位主要集中于下白垩统莱阳群的浊积岩,对下白垩统青山群未见详述。利用野外露头与镜下薄片资料,详细描述了灵山岛地区下白垩统青山群的岩性特征、岩相组合、软沉积物变形构造类型与特征,指出研究区青山群软沉积物变形构造主要宿主岩层为陆相扇三角洲沉积,其沉积水体逐渐变浅,并伴随多次火山爆发。软沉积物变形构造类型主要有负载构造、球—枕构造、泄水构造、挤入构造、水塑性褶皱、塑性砂岩团块包卷构造、火山地震落石构造和“V”型地裂缝等,形成原因主要为火山爆发引起的古火山地震作用,成因机制主要分为地震波、火山碎屑物重力及惯性作用与瞬时差异气压效应3种,这与莱阳群浊积岩层位的软沉积物变形构造主要为滑塌与构造古地震机制不同。通过分析火山碎屑流堆积层位与软沉积物变形构造发育层位的关系,建立了青山群软沉积物变形构造的分布模式,即随着与火山口距离的变化,近源易见的脆性变形逐渐消失,中源以液化软沉积物变形与塑性变形为主体,远源呈现弱的液化软沉积物变形,且软沉积物变形构造的规模与距离呈负相关。

关键词: 灵山岛, 下白垩统, 青山群, 软沉积物变形构造, 火山地震

Abstract: Recently,the study on the soft-sediment deformation structures(SSDS) of Lingshan Island is a hot topic. The research is focused on the SSDS in turbidite system of the Lower Cretaceous Laiyang Group, while specific study on the SSDS in fan delta system of the Lower Cretaceous Qingshan Group is not illustrated in details. With the field outcrops and thin sections,we analyzed the lithologic characteristics,lithofacies associations, classification and characteristics of SSDS of the Lower Cretaceous Qingshan Group in the study area. A conclusion was acquired that the palaeoenvironment is a fan delta system with several volcanic eruptions,and the water became shallower gradually. The types of SSDS include load structure,ball and pillow structure,water escape structure, sediment-injection structure,hydroplastic deformation,plastic sandstone breccia,volcanic drop stone and “V”shaped ground fissure. They were mainly caused by volcanic earthquakes of three types: seismic wave,the gravity and inertia effect of pyroclastic deposition and instant differential air pressure,which are different from the slumping and tectonic earthquake occurred in the Laiyang Group. In addition,with the analysis of association between the pyroclastic flows and the SSDS horizons,a distribution model of SSDS related to volcanic earthquake can be built: The types of SSDS range gradually with the variation of distance from volcanic vent. The brittle deformation structure, common type in proximal zone, disappears gradually; in the medial zone, liquefied and plastic SSDS become dominant types; while in distal zone, slightly liquefied SSDS develops. Additionally,the scale and size of SSDS is negatively correlated with the distance from the volcanic vent.

Key words: Lingshan Island, Lower Cretaceous, Qingshan Group, soft-sediment deformation structure, volcanic earthquake

中图分类号:

P512.2

周瑶琪, 周腾飞, 张振凯, 梁钊, 梁文栋, 王安东, 于姗姗. 山东省灵山岛下白垩统青山群火山地震软沉积物变形构造特征及成因机制^*[J]. 古地理学报, 2017, 19(4): 567-582.

Zhou Yaoqi, Zhou Tengfei, Zhang Zhenkai, Liang Zhao, Liang Wendong, Wang Andong, Yu Shanshan. Characteristics and formation mechanism of soft-sediment deformation structures related to volcanic earthquakes of the Lower Cretaceous Qingshan Group in Lingshan Island, Shandong Province[J]. JOPC, 2017, 19(4): 567-582.

http://www.gdlxb.cn/CN/Y2017/V19/I4/567

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Characteristics and formation mechanism of soft-sediment deformation structures related to volcanic earthquakes of the Lower Cretaceous Qingshan Group in Lingshan Island, Shandong Province

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Characteristics and formation mechanism of soft-sediment deformation structures related to volcanic earthquakes of the Lower Cretaceous Qingshan Group in Lingshan Island, Shandong Province

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