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江西彭山隐伏花岗岩是1967年开展地质普查和矿产预测时发现的.围绕岩体外接触带探明了中-大型的隐伏夕卡岩型锡石硫化物矿床,远离接触带找到了初具规模的云英岩型锡石矿床. 该岩体具有我国南方湘、粤、桂、滇同类酸性含锡花岗岩岩石的共同特点,但在酸度、碱度、潜在含矿性和岩浆分异作用诸方面又有独特之处.
The Pengshan concealed granite in Jiangxi Province was discovered during geological survey and mineral prediction carried out in 1967. The medium-large concealed skarn-type cassiterite deposits have been found around the outer contact of the rock mass and have taken shape far away from the contact zone Of the Yunyingyan type cassiterite deposit.The rock mass has the common features of the same acidic tin-bearing granite rocks in southern Hunan, Guangdong, Guangxi and Yunnan, but in acidity, alkalinity, potential ore-bearing and magmatic differentiation Another unique.