|Table of Contents|

Comparisons of the Collision Processes and Related Metallogenesis of Zagros and Himalaya Orogens(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2021年第03期
Page:
436-448
Research Field:
院士专稿
Publishing date:

Info

Title:
Comparisons of the Collision Processes and Related Metallogenesis of Zagros and Himalaya Orogens
Author(s):
ZHANG Hong-rui* HOU Zeng-qian**
(Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China)
Keywords:
collisional orogen collision process metallogenesis ore-forming structure juvenile crust Zagros Himalaya Tibetan Plateau
PACS:
P56
DOI:
10.19814/j.jese.2020.11001
Abstract:
The study on continental collision process will shed light on plate tectonics within continent. However, there are some problems about the timing of the initial collision, such as the division about collisional phases and the dynamics of collisional metallogenesis. Comparing Zagros and Himalayan orogens in terms of their deformation, magmatism, and metallogenesis, it is noted that there is a time lag between intense collisional related shorting and initial collision. In the meanwhile, arc-like magmatic activity can also occur within collisional continental zone. It is suggested that the lag time between tectonic-magmatic activities and initiation of continental collision reflects the effects of a collision process involving the “soft” collision. Thus the collision processes can be divided into three phases, including soft collision, hard collision, and post collision. Among them, the soft collision phase is characterized by low-rate contractional deformation and magmatism related to subducted oceanic slab. In contrast, high-rate contractional deformation and magmatism related to subduction of continental lithosphere occur during the hard collision phase. There are lots of extensional structures during post collision phase, and magmatic activity of this phase is mainly induced by delamination, breakoff and tearing of the continental lithosphere. The hydrothermal Pb-Zn ore deposits occur in the fold and thrust belt during soft and hard collision phases. The porphyry Cu deposits are controlled by large strike-slip faults during hard and post collision phases, whereas the detachment-fault-related polymetallic deposits form related to crustal extension during post collision phase. The juvenile crust form during the early subduction phase and subsequent collisional phase, and supply metal for ore-forming system within continental collision zones.

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Last Update: 2021-05-01