摘要
通过对马来西亚吉兰丹州兰道班江铁矿地质特征的研究,认为成矿热液来源于中酸性花岗闪长岩体,地层为碳酸盐类,二者发生接触交代作用形成矽卡岩型铁及多金属矿床。
Through the study of geologic features of Landau Banjiang iron deposit,Kelantan,State of Malaysia,it is considered that ore-forming hydrothermal solution derived form neutral and acidic granodiorite,which belongs to carbonate rock.In contact metasomatism,formed skarn type iron and polymetallic ore deposit.
出处
《吉林地质》
2009年第2期52-55,共4页
Jilin Geology
关键词
铁及多金属矿床
地质特征
兰道班江
马来西亚
iron and polymetallic ore deposit
geologic feature
Landau Banjiang
Malaysia
