构造-流体耦合有限元模拟:以石英脉型钨矿为例

刘向冲

doi:10.12090/j.issn.1006-6616.2019.25.S1.028

构造-流体耦合有限元模拟:以石英脉型钨矿为例

doi: 10.12090/j.issn.1006-6616.2019.25.S1.028

刘向冲^{1, 2,}

1.
中国地质科学院地质力学研究所, 北京 100081
2.
中国地质科学院地质力学研究所动力成岩成矿实验室, 北京 100081

基金项目:

国家自然科学基金 41602088

中国地质科学院基本科研业务费 JYYWF20180602

中国地质科学院基本科研业务费 DZLXJK201603

详细信息

作者简介:
刘向冲(1987-), 男, 副研究员, 从事成矿动力学数值模拟和数学地质等研究。E-mail:xcliu@cags.ac.cn

中图分类号: P612;P541
计量
- 文章访问数: 358
- HTML全文浏览量: 203
- PDF下载量: 16
- 被引次数: 0
出版历程
- 刊出日期: 2019-05-01

FINITE-ELEMENT SIMULATIONS OF STRUCTURE-FLUID COUPLING: A CASE STUDY IN VEIN-TYPE TUNGSTEN DEPOSITS

LIU Xiangchong^{1, 2
,}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
The Laboratory of Dynamic Digenesis and Metallogenesis, Institute of Geomechanics, CAGS, Beijing 100081, China

摘要

摘要: 热液矿床成矿作用动力学过程涉及多时空高度耦合的物理和化学过程。数值模拟是研究这一复杂动力学过程的重要而有效的工具之一，也可在找矿预测等方面发挥重要作用。以南岭地区石英脉钨矿床为例，利用计算机求解控制构造-流体的物理和化学方程，定量揭示成矿热液聚焦流动与"五层楼"成矿的对应关系，正演高压成矿流体致使围岩发生水力破裂及其成矿效应。模拟结果与石英脉型钨矿床的构造地球化学特征相符。
- 钨矿 /
- 数值模拟 /
- 聚焦流动 /
- 五层楼 /
- 水力破裂 /
- 黑钨矿沉淀 /
- CO₂逃逸
Abstract: The dynamic process of hydrothermal ore-forming involves highly coupled physical and chemical processes at different spatial and temporal scales. Numerical simulation is one of important and effective tools to decipher these complex processes and aids in prospecting. The vein-type tungsten deposits in the Nanling Range are taken examples to show how to solve the physical and chemical equations controlling the coupled structure-fluids using numerical simulation, decipher the relationships between fluid focusing and the tungsten mineralization in the five-floor vertically morphological zonation quantitatively, and reproduce the influences of hydraulic fracturing driven by high-pressure fluids on wolframite precipitation. The numerical results are consistent with the geochemical characteristics constrained by previous studies.
- tungsten deposits /
- numerical simulation /
- fluid focusing /
- five-floor zonation /
- hydraulic fracturing /
- wolframite precipitation /
- CO₂ escaping

HTML全文

图 1 石英脉型钨矿床成矿流体流动二维模型

Figure 1. A two-dimensional model of hydrothermal flow at vein-type tungsten deposits

下载: 全尺寸图片幻灯片

图 2 数值模拟实验1的流速场(m/s)

Figure 2. The distribution of fluid velocity in the experiment 1(m/s)

下载: 全尺寸图片幻灯片

图 3 截取4 km深处100 m×100 m的水力破裂二维模型

Figure 3. A 100 m×100 m two-dimensional model of hydraulic fracturing at a depth of 4 km

下载: 全尺寸图片幻灯片

图 4 施加流体附近节点在水力破裂后应力场和流体压力变化

Figure 4. The change of the stress and fluid pressure after hydraulic fracturing at a reference node closed to the fixed fluid pressure

下载: 全尺寸图片幻灯片

表 1 数值模拟实验1各个单元的水力学参数

Table 1. Hydraulic parameters of each unit in the experiment 1

参数	岩体	S1	S2	S3, S4	S5, S6, S7
渗透率/m²	1.0×10^-18	1.0×10^-16	2.0×10^-16	7.0×10^-14	3.0×10^-15
孔隙度	0.0015	0.015	0.02	0.14	0.05
箭头代表流体流动的方向，底部数值是最高流速。

下载: 导出CSV

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