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《Journal of Chengdu University of Technology(Science & Technology Edition)》 1986-02
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THE TECTONIC ENVIRONMENT AND AGE OF THE OPHILITES IN EAST QLNLING

Tang Yaoqing;Lu Yilun Institute of Geology, Chinese Regional Geological Academy of Geological Sciences Survey Team of Shanxi Province  
East Qinling ophiolitic belt is located in the ancient island--arc ofQinling early Paleozoic orogenic belt bettween the North China Massif andthe Yangtse Massif. The ophiolite sequences are re--established from bottom to top asfollows: 5. silicolites 4.mafic volcanic rocks 3. cumulative complex 2. metamorphic peridotites 1. metamorphic aureole Metamorphic Peridotites are rech in Cr, Ni and poor in Al andalkali, and represent the partial melting remnants of the mantle. During the fractional crystallization, iron is apparently concentratedin the cumulative complexes. Geological features and petrochemical characteristics of the ophiolitesand mafic lavas show that the ophiolite in East Qinling might be formedin a environment of marginal sea or small ocean basin between NorthChina Massif and Qinling ancient island--arc. East Qinling ophiolite formed in early Paleozoic (probably in earlySilurian), emplaced and obducted on the ancient island--arc at the end ofearly Paleozoic.
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