雄安新区浅地表地质—地球物理三维可视化建模

doi:10.11720/wtyht.2025.0101

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摘要

构建重点城市区三维可视化模型是实现多学科资料交叉融合、直观展示地层空间展布特征的重要手段。本文综合运用地球物理数据开展三维可视化模型构建,解决已有三维模型在地质—地球物理综合解释和成果具象展示等方面存在的不足。通过构建雄安核心区5 km以浅的三维构造模型和三维速度模型,揭示了三维S波速度分布特征对地层空间形态的响应,验证了雄安核心区凸起和凹陷相间发育的构造格局。0~1 km深度范围内,S波速度的横向均匀性反映了第四系和新近系地层的稳定沉积特征;1~2.2 km内,速度分带效应不明显,主要由于蓟县系热储层裂隙发育导致S波速度降低;2.2 km以深,徐水凹陷与容城凸起构造单元间显著的速度对比主要源于岩性差异及地层的不整合接触。通过构建三维速度模型,有助于突破有限地质资料的局限,从物理属性角度揭示雄安核心区地下三维结构的特征。

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	朱帅鹏
	邱勇
	徐志萍
	刘巧霞
	林吉焱
	段永红
	李菊红

关键词 ：三维建模, 三维S波速度模型, 雄安新区, 地球物理数据, SKUA-GOCAD

Abstract：

The construction of three-dimensional visualization models in key urban areas is important for multidisciplinary data integration and intuitive presentation of spatial stratigraphic distribution.However,existing models face limitations in integrated geological-geophysical interpretation and concrete visualization of results.In response to this,this study established a 3D visualization model based on comprehensive geophysical data,specifically including a 3D structural model and a 3D velocity model for the Xiong'an core area down to 5 km depth.It revealed the correspondence between the 3D S-wave velocity distribution and the spatial morphology of strata,and validated the structural framework of alternating uplifts and depressions.To be specific,within the depth range of 0~1 km,the lateral homogeneity of S-wave velocity reflects the stable sedimentary characteristics of Quaternary and Neogene strata.Between 1 km and 2.2 km,the velocity zoning is unclear,primarily due to fracture development in the Jixianian geothermal reservoir,which leads to a reduction in S-wave velocity.Below 2.2 km,the significant velocity contrast between the Xushui Depression and the Rongcheng Uplift is mainly attributed to lithological differences and unconformable contacts.The construction of the 3D velocity model helps overcome the limitations of sparse geological data and reveals the subsurface 3D structures in the Xiong'an core area from a physical property perspective.

Key words： 3D modeling 3D S-wave velocity model Xiong'an New Area geophysical data SKUA-GOCAD

收稿日期: 2025-04-14 修回日期: 2025-09-22 出版日期: 2025-12-20

ZTFLH:

P631

基金资助:国家自然科学基金(42374073);河南省自然科学基金面上项目(242300421374);中国地震局地球物理勘探中心青年基金项目(YFGEC2023011)

引用本文:

朱帅鹏, 邱勇, 徐志萍, 刘巧霞, 林吉焱, 段永红, 李菊红. 雄安新区浅地表地质—地球物理三维可视化建模[J]. 物探与化探, 2025, 49(6): 1333-1342.
ZHU Shuai-Peng, QIU Yong, XU Zhi-Ping, LIU Qiao-Xia, LIN Ji-Yan, DUAN Yong-Hong, LI Ju-Hong. 3D visualization modeling of shallow-surface geological and geophysical data in Xiong'an New Area. Geophysical and Geochemical Exploration, 2025, 49(6): 1333-1342.

链接本文:

https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2025.0101 或 https://www.wutanyuhuatan.com/CN/Y2025/V49/I6/1333

Fig.1 雄安新区大地构造
图中构造单元划分据何登发等^[18]修改,断层展布据商世杰等^[20]修改,黑色矩形为雄安核心区域,浅蓝色线条为河流迹线

Table 1 建模数据来源

Fig.2 研究区数据资料分布
黑色矩形为雄安核心区域,AB红色线段为图切剖面位置

Fig.3 雄安核心区三维地质体模型

Fig.4 雄安核心区三维地质底界面模型

Fig.5 雄安核心区地质底界面与断层面三维展布

Fig.6 雄安核心区三维速度结构模型纵向切片

Fig.7 三维S波速度提取(2.5 km/s≤v_s≤2.6 km/s)

Fig.8 三维S波速度提取(2.7 km/s≤v_s≤3.3 km/s)

Fig.9 雄安核心区三维速度结构模型东西向垂直切片
图中黑色实线为剖面所过钻井,黑色波浪线为不整合界面

Fig.10 雄安核心区三维地质体模型东西向垂直切片

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