地球学报
地毬學報
지구학보
ACTA GEOSCIENTIA SINICA
2013年
z1期
163-167
,共5页
铝土矿床%地质特征%控矿因素%成矿规律%滇中
鋁土礦床%地質特徵%控礦因素%成礦規律%滇中
려토광상%지질특정%공광인소%성광규률%전중
bauxite deposit%geological characteristics%ore-control factor%metallogenesis%central Yunnan
通过对滇中地区典型铝土矿(老煤山铝土矿)成矿地质特征研究,认为该区铝土矿为古风化壳沉积型铝土矿,主要受地层层位、岩性古地理条件、褶皱构造及后期抬升改造影响。研究认为该区具有一定勘探潜力。
通過對滇中地區典型鋁土礦(老煤山鋁土礦)成礦地質特徵研究,認為該區鋁土礦為古風化殼沉積型鋁土礦,主要受地層層位、巖性古地理條件、褶皺構造及後期抬升改造影響。研究認為該區具有一定勘探潛力。
통과대전중지구전형려토광(로매산려토광)성광지질특정연구,인위해구려토광위고풍화각침적형려토광,주요수지층층위、암성고지리조건、습추구조급후기태승개조영향。연구인위해구구유일정감탐잠력。
Based on a study of metallogenic geological characteristics of the Laomeishan bauxite deposit, a typical bauxite deposit in central Yunnan, the authors hold that the bauxite deposits in this area are paleo-weathering crust sedimentary deposits controlled mainly by stratigraphic horizon, lithofacies-paleogeographical conditions, folded structure and late stage uplift and reformation. It is held that there exists certain exploration potential in this area.