|Table of Contents|

Constraints of Mazongshan Devonian Granites on the Tectonic Evolution of the Paleo-Asian Ocean in Beishan Orogenic Belt, China(PDF)

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

Issue:
2025年第01期
Page:
1-15
Research Field:
基础地质与矿床地质
Publishing date:

Info

Title:
Constraints of Mazongshan Devonian Granites on the Tectonic Evolution of the Paleo-Asian Ocean in Beishan Orogenic Belt, China
Author(s):
YU Ji-yuan1; 2; 3*;  WANG Guo-qiang1; 2;  JI Bo1; 2; 3;  BU Tao1; 2; 3;  LI Ting1; 2;  GUO Lei1
(1. Xi'an Center of Geological Survey, China Geological Survey(Geosciences Innovation Center of Northwest China), Xi'an 710119, Shaanxi, China; 2. Orogen Research Center of Geological Survey, China Geological Survey, Xi'an 710119, Shaanxi, China; 3. Strata Type Section for the Bottom of Wenlock-Shaanxi Ziyang Field Scientific Observation, Xi'an 710119, Shaanxi, China)
Keywords:
tectonic-magmatic evolution;  geochemistry;  granite;  zircon U-Pb age;  genesis;  Devonian;  Beishan orogenic belt
PACS:
P581
DOI:
10.19814/j.jese.2024.07031
Abstract:
There are great differences in tectonic evolution and tectonic unit division of Beishan orogenic belt. The key is that there is no unified understanding of the tectonic background during Devonian. In order to deepen the understanding of Paleozoic tectonic evolution in Beishan area, Mazongshan Devonian granite was selected for geochronology and geochemistry research. The K-rich, Na-poor and K-rich calc-alkaline series have the characteristics of peraluminous S-type granite. The A/CNK values are all greater than 1.1, and the differentiation of light and heavy rare earth elements is obvious.(La/Yb)N is 3.61-49.69, with slight Eu anomaly(δEu is 0.18-1.20), enrichment of Cs, Rb, Ba, Th, U and K, depletion of Nb, Ta, P and Ti, LA-ICP-MS zircon U-Pb age of(396.3±3.5)Ma, showing the granite forms in Early Devonian. Judging from the nature of its source area, the source area of the granite body is dominated by greywacke. According to the discrimination diagrams of granite genetic types such as Zr +Nb+Ce+Y-(K2O+Na2O)/CaO and Zr+Nb+Ce+Y-FeOT/MgO, it can be seen that Mazongshan monzongranite is S-type granite, which is formed in the tectonic environment of syn-collision and post-collision. The age, geochemical characteristics and formation environment of Mazongshan monzongranite confirm that the subduction process ends during Early Devonian in Early Paleozoic tectonic evolution of Beishan orogenic belt, and the region has entered the post-collision stage.

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Last Update: 2025-01-20