中文摘要：

铜陵地区中酸性侵入岩可划分为橄榄安粗岩系列和高钾钙碱性系列。前者岩石组合为辉石二长闪长岩＋二长岩＋石英二长岩,后者为辉长闪长岩＋石英二长闪长岩＋花岗闪长岩。两个系列岩石的组成矿物种类相似,但在不同岩石中的含量不同,主要造岩矿物为斜长石、辉石、角闪石、黑云母、钾长石、石英。橄榄安粗岩系列岩石中含有大量的深源包体,包括辉石堆积岩包体、角闪石堆积岩包体和角闪石辉长质堆积岩包体,主要矿物为辉石、角闪石,其次为尖晶石、斜长石、磷灰石、金云母;高钾钙碱性系列岩石中含大量的微粒闪长质包体、镁铁质石英二长闪长质包体和富云母包体,主要矿物为斜长石、角闪石、黑云母。在考虑温压计使用条件的前提下,选择合适的温压计计算了两个系列侵入岩及包体形成的温压条件。结果表明,橄榄安粗岩系列侵入岩侵位深度（4～6km）略小于高钾钙碱性系列侵入岩（6～7km）,各种堆积包体形成于45～65km的深位岩浆房,微粒闪长质包体形成于12～15km的浅位岩浆房,镁铁质石英二长闪长质包体是早期侵入岩的边缘相,而富云母包体可能为地壳部分熔融的残余相。

英文摘要：

Mesozoic intermediate-acid intrusive rocks in Tongling area can be divided into two magmatic series,namely the shoshonitic series and the high-potassium （K） calc-alkaline series.The shoshonitic series is characterized by the association of pyroxene monzodiorites （PMD）＋monzonites（Mz）＋quartz monzonites（QM）,whereas the high-potassium calc-alkaline series has the association of gabbro-diorite （GBD）＋quartz monzodiorites （QMD）＋granodiorites（GD）.Rocks of these two series have a similar mineral association composed of feldspar,pyroxene,hornblende,biotite,potassium feldspar and quartz,but the content of these minerals is different.The cumulate enclaves such as pyroxene cumulate,hornblende cumulate and hornblende gabbro in the shoshonitic series rocks are composed mainly of pyroxene and hornblende and subordinately of spinel,feldspar,apatite and phlogopite,while micro-diorite enclaves,mafic quartz monzodiorite enclaves and mica-enriched enclaves in the high-potassium calc-alkaline series are mainly comprised of feldspar,hornblende and biotite.Taking into account the preconditions for the application of thermobarometry,the authors calculated the pressure and temperature conditions for the formation of the intrusive rocks and enclaves.The calculated results of all enclaves and intrusive rocks show that their average temperatures and pressures are 1 357℃ and 1.783 GPa for pyroxene cumulate,1 228℃ and 1.430 GPa for hornblende cumulate,1 214℃ and 1.300 GPa for hornblende gabbro cumulate,889℃ and 0.413 GPa for micro-diorite enclave,887℃ and 0.114 GPa for mafic quartz monzodiorite enclaves,1 096～1 043℃ and 0.167～0.115 GPa for shoshonitic series,and 844～784℃ and 0.211～0.193 GPa for high-potassium （K） calc-alkaline series,respectively.If these pressure values are converted into the depth according to 3.3 kbar/km,their corresponding depths are 45～65 km for all cumulate enclaves,12～15 km for micro-diorite enclaves and about 4 km for mafic quartz monzodiorite enclaves,4