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《Geochimica》 2001-01
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Sr-Nd-Pb isotope mapping of Late Mesozoic volcanic rocks across northern margin of North China Craton and implications to geodynamic processes

ZHOU Xin- hua1, ZHANG Guo- hui1, YANG Jing- hui1, CHEN Wen- ji 2, SUN Min3 (1. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2. Institute of Geology, China Seismological Bureau, Beijing 100029, China; 3. Depart  
Late Mesozoic volcanic rocks are extensively spread on both sides of northern margin of the North China Craton (NCC), where is the boundary between an Archean craton to the south and a Paleozoic orogenic belt, Xing an- Mongolia Orogenic Belt (XMOB), to the north. Two major east- west trending faults, Kaiyuan- Chifeng Fault (KCF) and Xar Moron He Fault (XHF) develop in this margin zone as a boundary between two tectonic domains. The volcanism has been thought to be the magmatic response to the west- , or northwest- dipping subduction of Izanagi Plate and covers a wide range in lithologies, from rhyolites, dacites, trachyte, andesites to basalts. To clarify the role of underlain lithosphere in magma genesis, a systematic Sr- Nd- Pb isotope survey has been taken on these selected samples that contain SiO2 60% , i.e. basalt, trachyandesite and basaltic andesite. The results show a distinctive and contrasting pattern of isotope signatures on two sides of the boundary faults, KCF and XHF. A remarked EMI signature and EMI- PM mixing trend feature the isotope system of basaltic volcanism on the southern side, the North China Craton, whereas the primitive to slightly depleted signature dominates that of basaltic volcanism on the northern side, the Paleozoic Orogenic Belt (XMOB). A clearly transitional and variable signature has been shown in the area between two parallel EW trending faults, i.e. KCF and XHF. This picture is quite consistent with the available geological and geophysical observations. A chemical zoning of subcontinental mantle beneath eastern China (Zhou and Zhu, 1992) has shown the EMI affinity of sub- cratonic mantle based on a chemical inversion study of the Cenozoic mantle- derived rocks. However, a positive argument is presented to show that the magma sources of Mesozoic volcanic rocks in the region have been highly influenced by the underlain lithosphere although the magma has been evolved to different degrees. Furthermore, the results would support an alternative interpretation, reactivation of paleo- subduction zone, for the genesis of Mesozoic volcanic magmatism in this craton marginal area.
【Fund】: 国家自然科学基金资助项目!( 49733110);; 香港 RGC资助项目! (HKU7110/97P);; 科学技术部资助项目! (G1999057704)
【CateGory Index】: P597
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