Numerical modelling of gravitational sinking of anhydrite stringers in salt (at rest)

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Bollettino Di Geofisica Teorica Ed Applicata Pub Date : 2016-01-01 DOI:10.4430/BGTA0178
Shiyuan Li, J. Urai
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引用次数: 3

Abstract

A large number of salt bodies contain layers of anhydrite material which is generally referred to as “stringers”. The movement and deformation of embedded anhydrite bodies are processes which are not yet fully understood. It is observed that stringers tend to sink towards the bottom of salt bodies at velocities highly dependent on the mechanical properties of both salt and anhydrites, with given density contrast between salt and denser anhydrites. The rheological differences between salt and the embedded anhydrites are a major issue, contributing to the complexity of the problem. On a geological timescale, the salt behaves as a Newtonian or a power-law fluid. The anhydrite stringers present elastic or brittle properties under certain conditions. Finite Element Modelling (FEM) has been employed in this study by using the FEM package ABAQUS (SIMULIA, Dassault Systems) in order to numerically simulate the sinking of an anhydrite stringer embedded in the salt. Furthermore, numerical modelling of isolated anhydrite stringers in salt at rest is compared with observations of stringers in seismic data. FEM simulation of the anhydrite stringer sinking and the gravitational sinking of anhydrite blocks embedded in the salt will be studied and demonstrated with two different methods of rheology, respectively. The study results indicate that sinking velocity is closely related to several factors, including the viscosity, the thickness of the stringer, as well as the density contrast between stringer and salt for a given viscosity. The results also prove that anhydrite stringer fragments do not sink significantly over the geological timescale if the halite is deformed by non-Newtonian viscosity. But, when Newtonian viscosity is dominant, the fragments are likely to sink hundreds of metres through the Zechstein salt during a few Ma. In conclusion, the modelling of the sinking of anhydrite or anhydrite inclusions provides an important scope for understanding the movement and deformation of embedded stringers.
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硬石膏在盐中重力沉降的数值模拟(静态)
大量的盐体含有硬石膏物质层,这种物质层通常被称为“硬石膏”。嵌埋硬石膏体的运动和变形是一个尚未完全了解的过程。可以观察到,在给定盐和密度更大的硬石膏的密度对比下,弦状物倾向于以高度依赖于盐和硬石膏力学性能的速度向盐体底部下沉。盐和包埋硬石膏之间的流变差异是一个主要问题,导致了问题的复杂性。在地质时间尺度上,盐表现为牛顿流体或幂律流体。硬石膏筋在一定条件下具有弹性或脆性。本研究采用有限元模拟软件ABAQUS (SIMULIA, Dassault Systems)对硬石膏管柱埋入盐中的沉降过程进行了数值模拟。此外,本文还将静息盐中孤立硬石膏弦条的数值模拟与地震资料中弦条的观测结果进行了比较。本文将分别采用两种不同的流变学方法对硬石膏柱状沉降和硬石膏块体嵌入盐中的重力沉降进行有限元模拟研究和论证。研究结果表明,沉降速度与黏度、管柱厚度、一定黏度下管柱与盐的密度差等因素密切相关。结果还证明,在非牛顿黏度作用下,硬石膏串状碎片在地质时间尺度上不会明显下沉。但是,当牛顿粘度占主导地位时,碎片可能会在几分钟内下沉数百米,穿过泽克斯坦盐。综上所述,对硬石膏或硬石膏包裹体下沉的模拟为理解埋置弦板的运动和变形提供了一个重要的范围。
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Bollettino Di Geofisica Teorica Ed Applicata
Bollettino Di Geofisica Teorica Ed Applicata 地学-地球化学与地球物理
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期刊介绍: The "Bollettino di Geofisica Teorica ed Applicata" is an international open access journal dedicated to the publication of original papers dealing with Deep Earth Geophysics, Near Surface Geophysics, Exploration Geophysics, Borehole Geophysics, Geodynamics and Seismotectonics, Seismology, Engineering Seismology, Geophysical Modelling, Geodesy, Remote Sensing, Seismic and Geodetic Networks, Oceanography, and their application in the fields of Energy, Natural Resources, Environment and Climate, Policies and Regulations, Risk and Security, Technological Development.
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