[HTML][HTML] Structure and composition of collisional orogen in the southeastern margin of Tibetan Plateau, China: Constraints from petrogeochemistry and geophysics

Y Wang, HR Zhang - Journal of Earth Science and Environment, 2021 - jese.chd.edu.cn
… low-Y rocks, and combined with the geological evolution history of this area, these two high-…
The mantle anisotropy in the southeastern margin of Tibetan Plateau shows SN to the north …

[HTML][HTML] 南北构造带北段上地幔各向异性特征

常利军, 丁志峰, 王椿镛 - 地球物理学报, 2016 - html.rhhz.net
… of seismic anisotropy to provide important constraints on deformation patterns of the crust
and lithosphere mantle … temporary seismic array and 122 published results from permanent …

[HTML][HTML] 中国大陆及邻区上地幔P 波各向异性结构

郭飚, 刘启元, 陈九辉, 贺日政, 李顺成 - 地球物理学报, 2012 - html.rhhz.net
… This implies that the direction of the mantle flow is consistent with the absolute plate motion.
The fast P-wave directions are parallel to the direction of the principal stress in central Tibet, …

[PDF][PDF] 斜向碰撞板塊前緣之下部岩圈動力流場側向變化

喬凌雲 - 2002 - ntur.lib.ntu.edu.tw
… short wavelength and timescale is not only … seismic anisotropy and P-wave delays in New
Zealand has been interpreted as implying widespread deformation in the underlying mantle

[HTML][HTML] 青藏高原东南缘三维S波速度和径向各向异性及泸定MS6.8和芦山MS7.0地震孕震环境探讨

孙回归, 王兴臣, 常利军 - 地球物理学报, 2024 - dzkx.org
… Crustal anisotropy and deformation of the southeastern Tibetan Plateau revealed by
seismic anisotropy of mylonitic amphibolites. Journal of Structural Geology, 159: 104605, doi: …

[HTML][HTML] 远震P 波接收函数揭示的张家口(怀来)-中蒙边境(巴音温多尔) 剖面地壳厚度与泊松比

龚辰, 李秋生, 叶卓, 张洪双, 李文辉, 贺传松, 李英康 - 地球物理学报, 2016 - dzkx.org
: 本文使用时间域迭代反褶积算法, 从张家口(怀来)-巴音温多尔一线布设的41 个宽频地震台站,
1 年期间记录的连续三分量数据中提取到高质量的P 波接收函数1844 个. 用H-κ 扫描方法获得了…

[HTML][HTML] 大尺度地幔动力学研究的现状和展望

钟时杰 - 地球物理学报, 2021 - html.rhhz.net
… as a result of mantle convection modulated by surface plate motion history in the last 100 …
explained by mantle flow that is driven by buoyancy associated with the mantle structure. …

[HTML][HTML] 龙门山地区类似2008 年汶川大地震滑坡物质河流卸载时间的定量估算

刘锋, 付碧宏, 杨顺虎 - 地球物理学报, 2013 - html.rhhz.net
earthquake needs to take 3100 years. This timescale is similar to the recurrence interval of
great seismic events (~3000 years) like the 2008 Wenchuan earthquake in central Longmen …

变形岩石的显微构造与岩石圈流变学

刘俊来 - 地质通报, 2004 - dzhtb.cgs.cn
… Models of seismic anisotropy in the deep continental … settings), rock flow at different time
scales from seconds to million … natural rock flow and effective dating of rock flow deformation at …

大数据时代的地球动力学数值计算方法回顾与展望

张贝, 陈石 - 地球与行星物理论评, 2021 - sjdz.org.cn
… We hope that the review can give a holistic perspective to understand the development
Reconciling surface plate motions with rapid three-dimensional mantle flow around a slab edge[J]…