摘要
Based on widespred collection for the previous research data and deep comprehension on the predecessors’ achievements,and careful observation of petrography and systematic investigation of petrology,petrochemistry,trace element as well as isotope geochemistry,the geological and geochemical characteristics of the Mesozoic magmatic rocks in the Tongling area have been summarized, and the petrogenesis discussed. The results are as follows: 1) the intrusive rocks show zonal distribution along with east-west deep faults and hypabyssal intrusive output,mainly controlled by multistage faults in different directions and propertiesl 2) according to Q-A-P diagram,the intrusive rocks can be divided into pyroxene diorite,quartz diorite and granodiorite,and all of the three kinds of intermediate-acid dioritic rocks are belong to high potassic calc-alkaline seriesl 3) the similar geochemical characteristics of trace elements,rare earth elements and Pb-Sr-Nd-O isotope for the three kinds of intrusive rocks indicate that the magma was originated from an enriched lithospheric mantle and assimilated by the crustal materials; 4) the magma was likely derived from different layers of the magma chamber which were zonally distributed in the lower crust and randomly ascended,intruded in pulse,connecting with deep faults induced by tectonic movements; and 5) the geotectonic background of the Mesozoic regional magmatic activities of Tongling area maybe inside of the continental plate.