东南亚艾劳山-红河异质剪切带的应变定位和地震特性

IF 2.9 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Junyu Li, Shuyun Cao
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引用次数: 0

摘要

应变局部化是形成地壳尺度剪切带的关键;然而,对变形特征及其对地震性能影响的系统分析仍然缺乏。本文对哀牢山—红河剪切带(assr - sz)的杂闪岩和花岗质糜棱岩进行了详细的野外观测、微观结构分析、矿物晶体学优选取向、流变学参数和地震性质等综合分析。预先存在的成分和力学各向异性显著影响ASRR-SZ的应变局部化。ASRR-SZ南部以地壳深熔为主要特征,提示这些区域可能是应变局部化的起始点。ASRR-SZ的应变特征表现在变形温度(~ 400 ~ 440℃、~ 470 ~ 500℃和~ 730℃三个范围)、差应力(集中在15.9 ~ 65.1 MPa)和应变速率(集中在10−13 ~ 10−11 s−1)。值得注意的是,应变局部化显著改变了岩石组构,进而影响岩石的地震性质。p波各向异性:AVp = 6.8%-17.9%,最大值。沿x轴的Vp)和白色小体(AVp = 3.4%-3.7%,最大值。沿着y轴的Vp)。花岗岩糜棱岩的地震速度和AVp与石英含量呈线性相关,变形条件对其取向影响较大。在地壳中下厚度~ 25 km范围内,花岗质糜棱岩、黑素体、白色小体、角闪岩、片岩的快、慢极化剪切波延迟时间分别为0.3 ~ 0.66 s、0.37 ~ 0.7 s、0.22 ~ 0.31 s。这些岩石沿ASRR-SZ的平均延迟时间(dt)解释了观测到的延迟时间(dt = 0.58 s)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Strain Localization and Seismic Properties in the Heterogeneous Ailaoshan-Red River Shear Zone, Southeast Asia

Strain Localization and Seismic Properties in the Heterogeneous Ailaoshan-Red River Shear Zone, Southeast Asia

Strain localization is crucial in developing crustal-scale shear zones; however, a systematic analysis of deformation characteristics and their impact on seismic properties is still lacking. This study provides a comprehensive analysis of migmatites and granitic mylonites in the Ailaoshan-Red River shear zone (ASRR-SZ), incorporating detailed field observations, microstructure analysis, mineral crystallographic preferred orientations, rheological parameters, and seismic properties. Pre-existing compositional and mechanical anisotropies significantly influence strain localization in the ASRR-SZ. The southern part of the ASRR-SZ is primarily characterized by crustal anatexis, suggesting these regions as potential initiation sites for strain localization. Strain characteristics in the ASRR-SZ manifest in deformation temperatures (three ranges, ∼400–440°C, ∼470–500°C, and ∼730°C), differential stress (concentrated at 15.9–65.1 MPa), and strain rate (concentrated at 10−13–10−11 s−1). Notably, strain localization significantly alters the rock fabric and further affects the seismic properties of rocks. Significant differences in Vp values and orientations are noted between melanosomes (anisotropy of P-waves: AVp = 6.8%–17.9%, Max. Vp along the X-axis) and leucosomes (AVp = 3.4%–3.7%, Max. Vp along the Y-axis). The seismic velocities and AVp in granitic mylonites exhibit a linear correlation with quartz content, and deformation conditions strongly influence their orientation. For a middle to lower crust thickness of ∼25 km, the delay times between fast and slow polarized shear waves are 0.3–0.66 s for granitic mylonites, 0.37–0.7 s for melanosomes, 0.22–0.31 s for leucosomes, 0.27–0.58 s for amphibolites, and 0.57–2.7 s for schists. The average delay time (dt) of these rocks along the ASRR-SZ accounts for the observed delay time (dt = 0.58 s).

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来源期刊
Geochemistry Geophysics Geosystems
Geochemistry Geophysics Geosystems 地学-地球化学与地球物理
CiteScore
5.90
自引率
11.40%
发文量
252
审稿时长
1 months
期刊介绍: Geochemistry, Geophysics, Geosystems (G3) publishes research papers on Earth and planetary processes with a focus on understanding the Earth as a system. Observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, biosphere, and solar system at all spatial and temporal scales are welcome. Articles should be of broad interest, and interdisciplinary approaches are encouraged. Areas of interest for this peer-reviewed journal include, but are not limited to: The physics and chemistry of the Earth, including its structure, composition, physical properties, dynamics, and evolution Principles and applications of geochemical proxies to studies of Earth history The physical properties, composition, and temporal evolution of the Earth''s major reservoirs and the coupling between them The dynamics of geochemical and biogeochemical cycles at all spatial and temporal scales Physical and cosmochemical constraints on the composition, origin, and evolution of the Earth and other terrestrial planets The chemistry and physics of solar system materials that are relevant to the formation, evolution, and current state of the Earth and the planets Advances in modeling, observation, and experimentation that are of widespread interest in the geosciences.
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