Zircon U-Pb and geochemical analyses for leucocratic intrusive rocks in pillow lavas in the Danfeng Group,north Qinling Mountains,China |
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Authors: | Yan QuanRen Chen JunLu Wang ZongQi Yan Zhen Wang Tao Li QiuGen Zhang ZongQing Jiang ChunFa |
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Institution: | (1) Institute of Geology, Chinese Academy of Geological Sciences (CAGS), Beijing, 100037, China;(2) Beijing SHRIMP Center, CAGS, Beijing, 100037, China;(3) Xi’an Institute of Geology and Mineral Resources, China Geological Survey, Xi’an, 710054, China |
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Abstract: | Field observation showed that there are many irregular leucocratic intrusive rocks in pillow lavas in the Danfeng Group in
the Xiaowangjian area, north Qinling orogenic belt. Photomicrographs indicated that the protoliths of those altered leucocratic
intrusive rocks are dioritic rocks. Geochemical analyses showed that pillow lavas have a range of SiO2 from 47.35% to 51.20%, low abundance of TiO2 from 0.97% to 1.72%, and percentages of MgO (MgO#=41–49). Chondrite-normalized REE patterns of pillow lavas are even, indicative of a weak differentiation between LREE and
HREE (La/YbN=1.52–0.99). N-MORB-normalized trace element abundances showed that pillow lavas are enriched in incompatible elements (e.g.,
K, Rb, and Ba). Leucocratic intrusive rocks in pillow lavas have a wide range of SiO2 from 53.85%–67.20%, low abundances of TiO2 from 0.51%–1.10%, and MgO (MgO#=40–51), and higher percentages of Al2O3 (13.32%–16.62%) and concentration of Sr (342–539 μg/g), ratios of Na2O/K2O (2–7) and Sr/Y (17–28). Chondrite-normalized REE patterns of leucocratic intrusive rocks showed highly differentiation between
LREE and HREE (La/YbN=12.26–19.41). N-MORB-normalized trace element abundances showed that leucocratic intrusive rocks are enriched in incompatible
elements (e.g., K, Rb, and Ba), and significantly depleted in HFSE (e.g., Nb, Ta, Zr and Ti), indicative of a relationship
to subduction. Isotopically, leucocratic intrusive rocks have a similar ε
Nd(t) (+7.45–+13.14) to that of MORB (+8.8–+9.7), which indicates that those leucocratic intrusive rocks sourced from depleted
mantle most likely. SHRIMP U-Pb analyses for zircon showed that those leucocratic intrusive rocks were formed at 442±7 Ma,
yielding an age of subduction in the early Paleozoic in the north Qinling orogenic belt.
Supported by the National Natural Science Foundation of China (Grant No. 40472119), the Programme of Excellent Young Scientists
of the Ministry of Land and Resourcesof China, the Ministry of Science and Technology of China (Grant Nos. 2002CB412608 and
2006BABOlAll), and the China Geological Survey (Grant Nos. 1212010633601 and 1212010611807) |
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Keywords: | Danfeng Group pillow lava leucocratic intrusive rock geochemistry and isotope SHRIMP U-Pb dating |
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