Results 11 to 20 of about 235 (147)
Redox state of subducted sediments controls porphyry copper mineralization along the Tethyan belt [PDF]
The Tethyan orogenic belt hosts numerous world-class porphyry copper deposits, with most forming during the Cenozoic continental collision and fewer during earlier Mesozoic subduction.
Huawei Li +3 more
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Syn-subduction basins bear significant implications to understand tectonic evolution of any fossil subduction zone. The late Paleozoic to early Mesozoic (Paleo-Tethyan) tectonics of the eastern and southeastern Tibetan Plateau (i.e., the Sanjiang ...
Mingjuan Liang +12 more
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We present new U-Pb detrital zircon ages, depositional history and tectonic model for the Liuqu Conglomerate (LQC) in southern Tibet that represents a critical geochronometer for the collision history of the Tibetan-Himalayan Orogenic Belt.
Yanxue Xie, Yildirim Dilek
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Late Cenozoic Evolution and Present Tectonic Setting of the Aegean–Hellenic Arc
The Aegean–Hellenic arc is a deformed sector of a long heterogeneous orogenic system (Tethyan belt), constituted by an inner old metamorphic crystalline core flanked by younger chains of European and African affinity, running from the Anatolian to the ...
Enzo Mantovani +3 more
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Metallogeny in the Bangong–Nujiang belt, central Tibet, China: A review
The Bangong–Nujiang metallogenic belt consists of scattered Tethyan oceanic blocks, mainly distributed underneath the margins of the Qiangtang and Lhasa terranes in central Tibet.
Yang Song +6 more
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Adakites or adakitic rocks usually show special geochemical signatures and are petrological probes to reveal the tectono–magmatic evolutionary history of paleo–orogenic belts. Here, we present a comprehensive study on the zircon U–Pb geochronology, whole-
Jie Gan +8 more
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The Zhangbaling tectonic belt is located in the middle segment of Dabie-Sulu Orogenic Belt and in the eastern part of the main segment of the Tan-Lu Fault Zone (TLFZ).
Qi Hou, Xiaoyong Yang, Mingjin Hou
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Temperature condition, sulfidation state, and gold formation mechanism of the Atash- Anbar polymetallic deposit (south Qazvin) based on mineralization, alteration and chemistry of ore minerals [PDF]
The NW-trending Urumieh-Dokhtar Magmatic Belt (UDMA) in the central-western Iran is a part of the Eastern Tethyan orogenic belt (Deng et al., 2018) and over past decades, it has become one of the most significant polymetallic (Au-Cu-Fe-Pb-Zn) provinces ...
Ebrahim Tale Fazel +2 more
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Initiation of new subduction zones is an integral part of Earth's plate tectonics regime. It is generally accepted that the negative buoyancy of sufficiently old oceanic lithosphere provides the primary driving force for subduction initiation.
Gaoxue Yang +6 more
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Geochemistry and tectonomagmatism setting of gabbroic bodies in South of Ramsar, West of Mazandaran Province: Evidence for Oceanic Island magmatism [PDF]
IntroductionIn the study area, in Guilan and Mazandaran provinces and the northern heights of the Alborz mountain range in northern Iran, several gabbroic and ultramafic assemblages of different ages have been reported.
Vahid Rezania ye Komachaly +2 more
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