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《Geochimica》 1989-04
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PETROCHEMISTRY AND ISOTOPE GEOCHEMISTRY OF HANNUOBA BASALTS AND DATONG VOLCANOS

Xie Guanghong Wang Junwen(Institute of Geochemistry, Academia Sinicz)M. Tatsumoto(U. S. Geological Survey, Denver, Colorado, 80225, USA)A. R. Basu(Department of Geological Sciences, University oj Rochester, Rochester, New York, 14627, USA)  
Both the Hannuoba Neogene basalts and Datong Quaternary volcanos belong to continental basalts controlled by the fault system in the lithosphere. The former shows straddle B-type associations of alkali basalts with characteristic synneusis structures and the latter is typical alkali basalts. The REE patterns for both of them are characterized by LREE enrichment. Very small variations in Sr, Nd and Pb isotopes are noticed in these rocks, with 87Sr/86Sr ranging from 0.703804 to 0.704974, ΣNd between +1.1 to +6.7 and 206Pb/204Pb, 207Pb/204Pb, 208Pb /204Pb being 17.175-17.947, 15.322-15.436 and 37.112-37.935, respectively. The low radiogenic Pb, together with high Sr and low Nd, is consistent with the observation that radiogenic Pb decreases progressively from the Pacific towards the East China Continent. The results show that the basaltic magma is derived from the upper mantle, with no contamination by crustal material, under the control of tensional back-arc tectonics, mantle uplifting, basin subsidence and deep fault systems.
【Fund】: 美国国家科学基金(NSF)
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