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《Acta Petrologica Sinica》 2005-05
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Qi JP,Zhang J and Tang GJ.2005.Carbon and oxygen isotope composition of the Meso-Neoproterozoic strata south of the Xiong'er terrane:evidence of the CMF model.

QI JinPing ZHANG Jing TANG GuoJun 1.Laboratory of Orogen and Crust Evolution,Peking Unirersity,Beijing 100871,China2.Key Laboratory for Metallogenic Dynamics,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences.Guangzhou 550002,China3.State Key Laboratory of Geological Processes and Mineral Resources,China Unirersity of Geoscieuces,Beijing 100083,China  
In terms of the CMF model (Tectonic Model for Collisional Orogeny,Metallogeny and Fluid Flow),former researchers inferred that the ore - forming fluids and metals of gold/silver deposits in the Xiong'er Terrane had been mainly sourced from intracontinental subduction - related metamorphic devolatilization of the Meso - Neoproterozoic strata (Guandaokou and Luanchuan Groups) south of the Xiong'er Terrane,and that the strata should be enriched in radiogenic Pb and Sr,and have high δ~(13)C and δ~(18)O values.To examine this inference and the CMF model,we have studied the Meso - Neoproterozoic strata and report the C and O isotope results in this paper.Thirteen δ~(18)O analyses of bulk-rock samples range 9.1‰~16.7‰ and average 13.3‰;four δ~(13)C_(CaCO_3) values range -2.8‰~0.8‰ and average -0.9‰.Calculations show that the δ~(18)O_w values of the fluids,supposed to be sourced from metamorphic devolatilization of the strata at temperature span of 320~373℃ (early-stage metallogenic temperature of most deposits in the Xiong'er Terrane),must be in the range of 2.6‰~14.6‰.The calculated δ~(18)O_w range,as interred by former researchers, fully covers the available δ_(18)O_w values of the early-stage ore-fluids in the Xiong'er Terrane (δ~(18)O_w=5.1‰~12.6‰).The calculated δ~(13)C_(CO_2) values for fluids originated from metamorphic devolatilization of the strata are between -0.7‰~4.0‰,consistent with the δ~(13)C_(CO_2) values (-2.1‰~4.0‰,mostly0 in early stage) of ore - forming fluid - systems in the Xiong'er Terrane. Therefore,our study strongly supports previous inference mentioned above and the science and utility of the CMF model.The CMF model can be employed to guide future exploration and geological study in the Xiong'er Terrane and comparable tectonic settings.
【Fund】: 本文得到自然科学基金项目(编号40425006 40352003和49972035);; 科学院百人计划项目(ZX 创303)的资助
【CateGory Index】: P597.2
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