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《SEISMOLOGY AND GEOLOGY》 2000-01
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A XENOLITH-DERIVED GEOTHERM FOR THE LOWER CRUST AND UPPER MANTLE BENEATH HANUOBA AREA, HEBEI PROVINCE, CHINA AND ITS GEOLOGIC IMPLICATIONS

Shi Lanbin Lin Chuanyong Chen Xiaode (Institute of Geology, China Seismological Bureau, Beijing 100029) (Laboratory of Tectonophysics, China Seismological Bureau, Beijing 100029) Han Xiuling (Institute of Geology, Chinese Academy of Sciences, Beiji  
A reliable geotherm has been constructed for the lower crust and upper mantle beneath Hanuoba, Hebei Province, China through the detailed study of xenoliths from basalts. The construted geotherm is higher than the oceanic geotherm and that for old cratonic areas. It is comparable to that for the eastern margin of Australian craton, and seems to indicate the tectonic regime of the studied area. The petrologic section derived from this geotherm indicates that the lower crust of this area consists mainly of granulite facies rocks of mafic compositions. They span from about 27km to 42km depth. The upper mantle consists of lherzolite, and it seems that there is a transition zone between spinel and garnet lherzolites. The crust mantle boundary defined by this geotherm is at 42km depth and coincides well with the seismic Moho. However, the overlapping of the equilibrium temperatures of some granulite and spinel lherzolite xenoliths indicates that granulite, spinel lherzolites and garnet pyroxynite may be interlayered in a zone above the crust mantle boundary. This may explain the layered reflectors observed at the base of lower crust. The lithosphere-asthenosphere boundary can be derived to be at about 95km depth, and the underlying asthenosphere consists of garnet lherzolite incorporated by upper mantle fluids. The obtained results may provide basic constraints for the lithosphere mapping and the construction of seismogenic model of the area.
【Fund】: 国家地震局“九五”重点项目!(950 4 0 80 4 0 1);; 地震科学联合基金!(196 0 30 )
【CateGory Index】: P58
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9 Gao Mingxiu;CURRENT TENSILE STRESS FIELD IN THE BLOCK- FAULTING TECTONIC AREAS OF NORTH CHINA[J];Seismology and Geology;1979-02
10 Ye Hong and Zhang Wenyu (Institute of Geology, State Seismological Bureau);THE CHARACTERISTICS OF INTRAPLATE EARTHQUAKE FAULTS IN NORTH CHINA AND THEIR RELATIONSHIP TO THE DYNAMICAL PROCESSES IN EARTH'S CRUST AND UPPERMOST MANTLE[J];Seismology and Geology;1980-01
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