地质找矿论丛2012，Vol.27Issue(3)：337-340,4.DOI:10.6053/j.issn.1001-1412.2012.03.012
印度尼西亚苏拉威西岛某红土型镍矿床地质特征及成因浅析
Geologic features and genesis of lateritic nickel deposits in Sulawesi island, Indonesia
摘要
Abstract
Base on the geologic feature and studies on the ore-forming condition it's considered that the deposit was formed from ultrabasic rocks, such as peridotite, During Mesozoic, Tertiary and Quaternary periods annual temperature and rainfall are both high in the area and rain and drought alternates. The ultrabasic rocks were weathered, and nickel leached and precipitated and enriched.关键词
红土型镍矿/地质特征/超基性岩/印度尼西亚Key words
Lateritic nickel deposits, geologic features, ultrabasic rocks, Indonesia分类
天文与地球科学引用本文复制引用
赖木收,马毅敏,林斌..印度尼西亚苏拉威西岛某红土型镍矿床地质特征及成因浅析[J].地质找矿论丛,2012,27(3):337-340,4.
