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《Journal of Changchun University of Science and Technology》 2003-01
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THE DEEP PROCESS OF FORMATION AND EVOLOTION OF SONGLIAO BASIN Mesozoic volcanic rock probe

WANG Qinghai, XU Wenliang(College of Earth Sciences, Jilin University,Changchun130026, China)  
The Mesozoic volcanism in Songliao basin revealed one aspect of the history of formation and evolution of Songliao basin. The petrological and geochemical data of Mesozoic volcanic rocks in Songliao basin indicate that the deep process of Mesozoic volcanisms is a counterclockwise PTt locus, which corresponds with the upward to downward drifts of magma sources. From late Jurassic to the early stage of early Cretaceous, the deep process of volcanisms is a falling pressure-temperature process, which corresponds with the graduall uplift of isothermal plane, the increase of lithospheric extension rate, the upward drift of magma sources, and the transformation of fault depression to depression in basin evolution. From the early stage of early Cretaceous to the late of early Cretaceous, the volcanism deep process is a increasing pressure-temperature process, which corresponds with the decrease of isothermal plane and lithospheric extension rate, the downward drift of magma sources and the depression stage of the basin evolution.
【Fund】: 中国石化公司"十五"重点攻关项目(P00002028);; 高校博士学科点基金项目(20010183007)
【CateGory Index】: P544.4
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