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《Chinese Journal of Geophysics》 2012-11
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Analysis on the thermal history and uplift process of Zijinshan intrusive complex in the eastern Ordos basin

CHEN Gang1,DING Chao1,XU Li-Ming2,ZHANG Hui-Ruo2, HU Yan-Xu1,YANG Fu1,LI Nan1,MAO Xiao-Ni1 1 State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi′an 710069,China 2 Changqing Oilfield Company,PetroChina Company Limited,CNPC,Xi′an 710021,China  
Thermochronological data of in-situ zircon U-Pb,hornblende and biotite 40Ar-39Ar,and zircon and apatite fission track(FT) are presented in this paper for studying the thermal history and uplift-cooling process of Zijinshan intrusive complex at the eastern margin of the Ordos basin in the central North China Craton(NCC).Alkaline intrusive rocks dominate the complex with the diopside monzonite and syenite as the dating samples in this work.Zircon U-Pb dating of the monzonite provides the initial crystallization age of the Early magmatic intrusion at 136.7 Ma,and 40Ar-39Ar dating of hornblendes and biotites indicates the late crystallization to solidification age of the emplaced magma to be mainly in a range of 133.1~130.4 Ma.A conclusion can be therefore drawn that the intrusive complex was mainly formed in 136.7~130.4 Ma of the Early Cretaceous.Based on the comprehensive analysis of the thermochronological T-t curve of the complex and the apatite FT modeling thermal path of the monzonite and altered sandstone,it can be further concluded that the uplift-cooling process of the Zijinshan complex and its intruded area of the eastern Ordos basin has experienced at least three tectono-thermal stages as follows:(1) the crystallization to consolidation stage of the magma emplacement during 136~120 Ma at an extremely high cooling rate of 52 ℃/Ma;(2) the slow uplift-cooling stage during 120~30 Ma at an average uplift-cooling rate of 2.5 ℃/Ma;and(3) the fast uplift-cooling stage initiated at 30~Ma with an average uplift-cooling rate of 3.6 ℃/Ma,accompanied by a more rapid uplift-cooling process since 10 Ma at an average rate of 7 ℃/Ma.Zijinshan magma intrusion in the eastern Ordos basin is an exhibition of the dynamic transformation and its related large-scale magmatism in NCC during Early Cretaceous.Then,the 2-stage differential uplifting processes are dynamically associated with far-field effects produced by synchronous convergences toward the central NCC of the(Paleo-) Pacific plate and Tethys or Indian plate at fluctuating subduction rates during Late Cretaceous to Neogene and Quaternary.
【Fund】: 国家重点基础研究(2003CB214607);; 国家自然科学基金(41002071);; 教育部高校博士点专项科研基金(20116101110006);; 国家留学基金(200721S073)与留学人员择优经费共同资助
【CateGory Index】: P542
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