The role of structural inheritance in continental break-up and exhumation of Alpine Tethyan mantle(Canavese Zone,Western Alps)     

Andrea Festa  Gianni Balestro  Alessandro Borghi  Sara De Caroli  Andrea Succo 《地学前缘(英文版)》2020,11(1):167-188

The Canavese Zone(CZ)in the Western Alps represents the remnant of the distal passive margin of the Adria microplate,which was stretched and thinned during the Jurassic opening of the Alpine Tethys.Through detailed geological mapping,stratigraphic and structural analyses,we document that the continental break-up of Pangea and tectonic dismemberment of the Adria distal margin,up to mantle rocks exhumation and oceanization,did not simply result from the syn-rift Jurassic extension but was strongly favored by older structu ral inheritances(the Proto-Canavese Shear Zone),which controlled earlier lithospheric weakness.Our findings allowed to redefine in detail(i)the tectono-stratigraphic setting of the Variscan metamorphic basement and the Late Carbonife rous to Early Cretaceous CZ succession,(ii)the role played by inherited Late Carboniferous to Early Triassic structures and(iii)the significance of the CZ in the geodynamic evolution of the Alpine Tethys.The large amount of extensional displacement and crustal thinning occurred during different pulses of Late Carbonife rous-Early Triassic strike-slip tectonics is wellconsistent with the role played by long-lived regional-scale wrench faults(e.g.,the East-Variscan Shear Zone),suggesting a re-discussion of models of mantle exhumation driven by low-angle detachment faults as unique efficient mechanism in stretching and thinning continental crust.  相似文献   

川东某场镇后山滑坡发育特征与机理分析     

陈世龙  郭伟  陈亚婷  张涛  刘晓钦 《四川地质学报》2020,40(1):119-124

四川盆地红层丘陵地区局部垂向裂隙发育的坡体容易受强降雨影响发生平推式滑坡,对于该类滑坡前人已有较为系统的研究,但对该类滑坡体局部复活特征的研究尚不深入。以川东某地老平推式滑坡体上发育的现代滑坡为例,分析了这类老滑坡局部复活的机理特征,5·12强震对滑坡体完整性造成了一定程度的破坏,是老滑坡复活的因素之一;但后缘人工弃渣的加载是其复活最直接的激发因素。文章对治理方案进行了可行性探讨,最终选用"前缘抗滑桩+后缘截水沟+裂缝夯实"方案。  相似文献   

藏南错那洞铍稀有多金属成矿时代:来自热液白云母Ar-Ar年龄的约束   总被引：2，自引：0，他引：2       下载免费PDF全文

梁维  李光明  张林奎  付建刚  黄勇  张志 《沉积与特提斯地质》2020,40(1):76-81

特提斯喜马拉雅是继华南和新疆阿尔泰之后又一条新发现的大型稀有金属成矿带,其成矿时代受到广泛的关注。本文以代表性矿床错那洞铍稀有多金属矿床为研究对象,挑选出矽卡岩型矿化体中的热液白云母,利用Ar-Ar同位素定年的方式测定热液活动时间,以此限制成矿时代。结果显示错那洞穹窿矽卡岩型矿体中白云母Ar-Ar同位素坪年龄为14.21±0.22Ma,对应的~(40)Ar/~(36)Ar-~(39)Ar/~(36)Ar的等时线年龄为14.21±0.27Ma,与错那洞穹窿中具有高分异特征的白云母花岗岩浆侵位时间(～14Ma)一致,表明错那洞矽卡岩型铍稀有多金属矿床的成矿年龄为～14Ma,而与穹窿内高分异白云母花岗岩一致的年龄暗示了该高分异花岗岩为该期矽卡岩型稀有金属矿化的成矿母岩浆。  相似文献   

西藏冈底斯南缘普夏洋岛的识别及其意义          下载免费PDF全文

张泽国  曾庆高  邓科  唐建科  何林武  袁仁华 《沉积与特提斯地质》2020,40(2):129-140

高出海平面的洋岛和低于海平面的海山是成熟大洋最重要的特征。笔者通过野外调查,于西藏自治区贡嘎县昌果乡普夏东侧的"原桑日群"中新识别出普夏洋岛。通对普夏洋岛的岩石学、地球化学研究及锆石U-Pb定年,认为普夏洋岛具有典型的"玄武岩+灰岩"岩石组合,其中的玄武岩为典型的洋岛玄武岩,形成于以成熟洋壳为基底的洋岛海山环境。普夏洋岛玄武岩的锆石U-Pb定年结果为203.9±1.6Ma和219.5±2.0Ma,表明其形成时代为晚三叠世。综合研究认为,普夏洋岛是雅鲁藏布江特提斯洋发现的较早的洋岛海山之一,证明雅鲁藏布江新特提斯洋在三叠纪已具有成熟的洋壳,普夏洋岛是雅鲁藏布江新特提斯洋向北俯冲形成的桑日群增生杂岩的重要组成部分。普夏洋岛的发现,丰富了新特提斯洋的研究内容,为反演研究区地质构造演化提供了新证据。  相似文献   

Mesozoic–Paleogene sedimentary facies and paleogeography of Tibet,western China: tectonic implications     

Kai‐Jun Zhang  Bangdong Xia  Xiwen Liang 《Geological Journal》2002,37(3):217-246

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