郯庐断裂带江苏段新生界三维地质构造建模

王金艳, 鲁人齐, 张浩, 李菊红, 李丽梅, 许汉刚, 顾勤平, 疏鹏, 侯莹

王金艳,鲁人齐,张浩,李菊红,李丽梅, 许汉刚,顾勤平,疏鹏,侯莹. 2020. 郯庐断裂带江苏段新生界三维地质构造建模. 地震学报,42(2):216−230. doi:10.11939/jass.20190131. DOI: 10.11939/jass.20190131
引用本文: 王金艳,鲁人齐,张浩,李菊红,李丽梅, 许汉刚,顾勤平,疏鹏,侯莹. 2020. 郯庐断裂带江苏段新生界三维地质构造建模. 地震学报,42(2):216−230. doi:10.11939/jass.20190131. DOI: 10.11939/jass.20190131
Wang J Y,Lu R Q, Zhang H,Li J H,Li L M,Xu H G,Gu Q P,Shu P,Hou Y. 2020. Three-dimensional geological modeling of Cenozoic erathem in Jiangsu segment of the Tanlu fault zone. Acta Seismologica Sinica42(2):216−230. doi:10.11939/jass.20190131. DOI: 10.11939/jass.20190131
Citation: Wang J Y,Lu R Q, Zhang H,Li J H,Li L M,Xu H G,Gu Q P,Shu P,Hou Y. 2020. Three-dimensional geological modeling of Cenozoic erathem in Jiangsu segment of the Tanlu fault zone. Acta Seismologica Sinica42(2):216−230. doi:10.11939/jass.20190131. DOI: 10.11939/jass.20190131

郯庐断裂带江苏段新生界三维地质构造建模

基金项目: 中国地震局星火科技项目(XH18016Y)、中国地震局地质研究所基本科研业务重点项目(IGCEA1602)、国家重点研发计划(2018YFC1504104)、新沂市活动断层探测与地震危险性评价项目和江苏省地震局青年科学基金(201802)共同资助
详细信息
    通讯作者:

    鲁人齐: e-mail:lurenqi@163.com

  • 中图分类号: P315.2

Three-dimensional geological modeling of Cenozoic erathem in Jiangsu segment of the Tanlu fault zone

  • 摘要:

    本文基于SKUA-GOCAD三维建模软件平台的构造-地层实体建模流程,通过整合研究区大量地质、地球物理资料和数据利用地质时间域坐标系转换和离散光滑插值(DSI)技术,并结合非定量化的地质基础利用地质网格功能建立了郯庐断裂带江苏段新生界的三维地质构造模型,该模型包括地表、第四系底部、新近系底部和基岩顶部等四个层面的地层模型和断层模型。该模型定量化地给出了研究区第四系、新近系底界的三维结构和特征,并刻画了主要活动断裂的三维空间分布,通过该模型可以更直观地显示研究区新生代地层单元和断裂的变化规律,对深入分析活动断裂带的沉积与构造具有重要的意义。

    Abstract:

    The establishment of three-dimensional geological structure model of active fault zones is an important basis for studying active faults, earthquake and geological disasters. Based on the tectonic-stratigraphic entity model flow of the 3D modeling platform SKUA-GOCAD, the UVT and DSI techniques in the geological time domain are used in this study. A 3D geological structure model of the Neogene in the Jiangsu segment of the Tanlu fault system is established, combined with the non-quantified geological foundation and the geological grid function. The three-dimensional model includes fault model and strata model with four layers (the surface, Quaternary bottom, Neogene bottom and bedrock top surface). The 3D model of Cenozoic erathem in Jiangsu segment of Tanlu fault zone gives the 3D structure and characteristics of Quaternary and Neogene basement quantitatively, and describes the 3D spatial distribution of main active faults. The three-dimensional model can more intuitively understand the Cenozoic stratigraphic units and faults in the studied area, which is of great significance to the in-depth analyses on the sedimentation and structure of active fault zones.

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  • 图  4   郯庐断裂带江苏段沿NE向(a)和SW向(b)的三维地质构造模型

    F1:山左口—泗洪断裂;F2:新沂—新店断裂;F3:墨河—凌城断裂;F4:窑湾—高作断裂;F5:马陵山—重岗山断裂

    Figure  4.   3-D geological structural models of the Jiangsu segment of the Tanlu fault zone along NE (a) and SW (b)

    F1:Shanzuokou-Sihong fault;F2:Xinyi-Xindian fault;F3:Mohe-Lingcheng fault;F4:Yaowan-Gaozuo fault; F5:Malingshan-Chonggangshan fault

    图  1   研究区地质构造简图

    F1:山左口—泗洪断裂;F2:新沂—新店断裂;F3:墨河—凌城断裂;F4:窑湾—高作断裂;F5:马陵山—重岗山断裂

    Figure  1.   Geological tectonic settings of the studied area

    F1:Shanzuokou-Sihong fault;F2:Xinyi-Xindian fault;F3:Mohe-Lingcheng fault;F4:Yaowan-Gaozuo fault; F5:Malingshan-Chonggangshan fault

    图  2   研究区资料和数据分布图

    Figure  2.   Data distribution map of the studied area

    图  3   构造-地层实体建模流程图

    Figure  3.   Flow chart of structure and stratigraphy modeling

    图  5   郯庐断裂带江苏段三维断裂模型

    Figure  5.   3D faults model of the Jiangsu segment of Tanlu fault zone

    图  6   研究区第四系底界地形(a)及第四系等厚线(b)

    Figure  6.   Quaternary bottom boundary (a) and Quaternary isopachs (b) in the studied area

    图  7   研究区地层二维剖面示意图

    Figure  7.   2D profile of strata in the studied area

    图  8   研究区地质构造剖面特征

    Figure  8.   Geological structure profile of the studied area

    图  9   研究区新近系底界地形(a)及新近系等厚线(b)

    Figure  9.   Neogene bottom boundary (a) and Neogene isopachs (b) in the studied area

    图  10   研究区基岩顶部三维地形图

    Figure  10.   3D topography on the topof the bedrock in the studied area

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出版历程
  • 收稿日期:  2019-07-28
  • 修回日期:  2020-01-13
  • 网络出版日期:  2020-05-21
  • 刊出日期:  2020-05-20

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