|Table of Contents|

Petrogenesis of Early Cretaceous Intrusive Rocks in Yinan Area of the Western Shandong, China: Implication for Crust-mantle Interaction Beneath North China Block(PDF)

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

Issue:
2022年第05期
Page:
723-749
Research Field:
基础地质与矿床地质
Publishing date:

Info

Title:
Petrogenesis of Early Cretaceous Intrusive Rocks in Yinan Area of the Western Shandong, China: Implication for Crust-mantle Interaction Beneath North China Block
Author(s):
GAO Ming-bo12 GAO Ji-lei12 ZHANG Yong-ming23* ZHANG Zhao-lu23 LIU Li-ping23 LI Ya-dong12 MA Ming12 LIU Xiao23 FENG Qi-wei12
(1. No.1 Geological Team of Shandong Provincial Bureau of Geology and Mineral Resources, Jinan 250014, Shandong, China; 2. Shandong Engineering Laboratory for High-grade Iron Ore Exploration and Exploitation, Jinan 250014, Shandong, China; 3. School of Resources and Environmental Engineering, Shandong University of Technology, Zibo 255000, Shandong, China)
Keywords:
geochemistry igneous complex zircon U-Pb age Sr-Nd-Pb isotope Hf isotope Early Cretaceous crust-mantle interaction Shandong
PACS:
P588.12; P597
DOI:
10.19814/j.jese.2021.11053
Abstract:
The Yinan area is located in the southeastern margin of North China Craton. There are lots of Late Mesozoic magmatic rocks in the area, which is an important case to study the North China Craton destruction and the intense crust-mantle interaction. Petrography, zircon U-Pb dating, geochemical and Sr-Nd-Pb-Hf isotope characteristics of the typical intrusive rocks in the area were carried out. The zircon U-Pb ages of quartz diorite and monzonite granite porphyry are(130.4±0.7)Ma and(129.5±0.6)Ma, respectively, indicating that the rocks form in Early Cretaceous. Geochemical characteristics show that the dioritic rocks are Na-rich but K-poor, belonging to cal-alkaline metaluminous series. The dioritic rocks are geochemically similar to high magnesian andesite/diorite and adakites. The rocks are enriched in LILEs and depleted in HFSEs. The chondrite-normalized REE patterns are right-inclined, LREE is steeper and HREE is gentler, there is no negative or weak Eu positive anomalies. The monzonitic granite porphyries are peraluminous and show high contents of Si and alkalis, low abundances of TFe2O3, MgO and CaO. The rocks are evidently depleted in Eu, belonging to highly differentiated I-type granite. Isotopic geochemical characteristics show that the εHf(t)values of the monzonitic granite porphyries are obviously lower than those of dioritic rocks. The dioritic rocks are more enriched in Pb isotopes than the monzonitic granite porphyries. Combined with the regional geological data, it is considered that Early Cretaceous intrusion in the area likely forms in the extensional background of the rotation of paleo-Pacific plate. The upwelling of the asthenosphere promotes partial melting of the overlying EM1+EM2 enriched mantles. The basaltic magma intrudes into the lower crust and mixes with the felsic magma in varying degrees in the lower crust to form dioritic magma. Felsic magma absorbs a small amount of mantle-derived basic magma, and experiences strong differentiation and evolution to form the monzonitic granite porphyries.

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Last Update: 2022-10-01