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《Chinese Journal of Geophysics》 1994-03
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DEEP TEMPERATURE AND LITHOSPHERIC THICKNESS LONG THE EASTERN SEGMENT OF THE HEISHUI─QUANZHOU GEOTRAVERSE

HU SHENG-BIAO; WANG JI-YANG (Institute of Geology,Academic Sinica. Beijing 100029)WANG YI-HUA(Nanjing University, Nanjing 210008)  
The experimental relationship between seismic velocity and radiogenic heat generation,in combination with the determined heat production for surface samples,was applied to evaluate the vertical distribution of heat sources for 18 seismic velocity depth profiles located along the Eastern segment of the Heishui-Quanzhou geotraverse. On this basis, the one-dimensional and two-dimensional steady-state heat conduction models along the geotraverse were constructed, and further more,the depth at which partial meltingbegin, i."thermal" lithospheric thickness, was estimated from the dry basalt solidus. The temperature field shows significant lateral variation, the temperatures at Moho range from 390 to 700℃, the corresponding"thermal" lithospheric thicknesses vary from 75 to 205 km, which is in good accordance with the results obtained from MTS. The differences between 1-D and 2-D models are most pronounced in the lower crust and upper mantle,where lateral heat transfer is remarkable. The temperature distribution along the peotraverse is related to the ages of the orogenses or of the superimposed thermalevents.
【Fund】: 国家自然科学基金
【CateGory Index】: P314.2
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