首页> 外文期刊>International Journal of Earth Sciences >Higher Himalayan Shear Zone, Sutlej section: structural geology and extrusion mechanism by various combinations of simple shear, pure shear and channel flow in shifting modes
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Higher Himalayan Shear Zone, Sutlej section: structural geology and extrusion mechanism by various combinations of simple shear, pure shear and channel flow in shifting modes

机译:Sutlej剖面的喜马拉雅山高剪切带:构造方式和挤压机制,通过简单剪切,纯剪切和转换模式下的河道流动的各种组合

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摘要

The Higher Himalayan Shear Zone (HHSZ) in the Sutlej section reveals (1) top-to-SW ductile shearing, (2) top-to-NE ductile shearing in the upper- and the lower strands of the South Tibetan Detachment System (STDS_U, STDS_L), and (3) top-to-SW brittle shearing corroborated by trapezoid-shaped minerals in micro-scale. In the proposed extrusion model of the HHSZ, the E_1-phase during 25-19 Ma is marked by simple shearing of the upper subchannel defined by the upper strand of the Main Central Thrust (MCT_U) and the top of STDS_U as the lower- and the upper boundaries, respectively. Subsequently, the E_(2a)-pulse during 15-14 Ma was characterized by simple shear, pure shear, and channel flow of the entire HHSZ. Finally, the E_(2b)-pulse during 14-12 Ma observed simple shearing and channel flow of the lower sub-channel defined by the lower strand of the Main Central Thrust (MCT_L) and the top of the STDS_L as the lower- and the upper boundaries, respectively. The model explains the constraints of thicknesses of the STDS_U and the STDS_L along with spatially variable extrusion rate and the inverted metamorphism of the HHSZ. The model predicts (1) shear strain after ductile extrusion to be maximum at the boundaries of the HHSZ, which crudely matches with the existing data. The other speculations that cannot be checked are (2) uniform shear strain from the MCT_U to the top of the HHSZ in the E_1phase; (3) fastest rates of extrusion of the lower boundaries of the STDS_U and the STDS_L during the E_(2a)- and E_(2b)-pulses, respectively; andrn(4) variable thickness of the STDS_L and rare absence of the STDS_U. Non-parabolic shear fabrics of the HHSZ possibly indicate heterogeneous strain. The top-to-SW brittle shearing around 12 Ma augmented the ductile extruded rocks to arrive a shallower depth. The brittle-ductile extension leading to boudinage possibly did not enhance the extrusion.
机译:Sutlej段的喜马拉雅山高剪切带(HHSZ)显示(1)藏南拆离系(STDS_U)的上,下股线的顶至西南延性剪切,(2)顶至NE延性剪切,STDS_L)和(3)由梯形矿物在微尺度上证实的从顶部到西南的脆性剪切。在建议的HHSZ挤压模型中,在25-19 Ma期间的E_1相的特征是对上主子通道的简单剪切,该子通道由主中心推力(MCT_U)的上链和STDS_U的上端定义为下端和下端。上限。随后,在15-14 Ma期间的E_(2a)脉冲的特征是整个HHSZ的简单剪切,纯剪切和通道流。最后,在14-12 Ma期间的E_(2b)脉冲观测到由主中心推力(MCT_L)的下部股和STDS_L的顶部分别作为下部和下部的下部子通道的简单剪切和通道流动。上限。该模型解释了STDS_U和STDS_L的厚度约束,以及空间可变的挤出速率和HHSZ的倒置变质。该模型预测(1)韧性挤压后的剪切应变在HHSZ的边界处最大,这与现有数据大致匹配。其他无法确定的推测是:(2)在E_1期从MCT_U到HHSZ顶部的均匀剪切应变; (3)分别在E_(2a)-和E_(2b)-脉冲期间,STDS_U和STDS_L的下边界的最快挤出速率; andrn(4)STDS_L的厚度可变,而STDS_U很少出现。 HHSZ的非抛物线剪切织物可能表明存在异质应变。大约12 Ma的从上到西南的脆性剪切增强了韧性挤压岩石的深度。脆性-延展性导致的松紧可能没有增强挤压。

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