云南勐海地区离子吸附型稀土矿控矿因素及找矿前景

P618.7; 云南勐海地区地处临沧-勐海(岩浆弧)Fe-Pb-Zn-Au-Ag-Sn-Sb-Ge-REE矿带(Ⅳ9)南段,近年来该区发现多个离子吸附型稀土矿床.为查明勐海地区离子吸附型稀土矿床控矿因素,指导后续找矿工作,本文在野外地质调查和室内综合整理分析的基础上,对勐海地区离子吸附型稀土矿床的成矿地质背景和成矿特征进行了初步研究,探讨了本区离子吸附型稀土矿床控矿因素与找矿前景.研究表明,勐海地区离子吸附型稀土矿床是以轻稀土为主的稀土矿,其成矿母岩为晚三叠世临沧花岗岩,次生富集成矿于新生代以来;其矿床的形成不仅受成矿母岩、地球化学、构造等内在因素的影响,亦受地形地貌、气候和植被等外在因素的控...

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Published in地质与勘探 Vol. 57; no. 4; pp. 935 - 946
Main Authors 蓝信杰, 张保涛, 卢文姬, 赵宪东, 李星亮, 王明波, 韩成, 王禹杰
Format Journal Article
LanguageChinese
Published 中国冶金地质总局山东正元地质勘查院,山东济南 250101 01.07.2021
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Abstract P618.7; 云南勐海地区地处临沧-勐海(岩浆弧)Fe-Pb-Zn-Au-Ag-Sn-Sb-Ge-REE矿带(Ⅳ9)南段,近年来该区发现多个离子吸附型稀土矿床.为查明勐海地区离子吸附型稀土矿床控矿因素,指导后续找矿工作,本文在野外地质调查和室内综合整理分析的基础上,对勐海地区离子吸附型稀土矿床的成矿地质背景和成矿特征进行了初步研究,探讨了本区离子吸附型稀土矿床控矿因素与找矿前景.研究表明,勐海地区离子吸附型稀土矿床是以轻稀土为主的稀土矿,其成矿母岩为晚三叠世临沧花岗岩,次生富集成矿于新生代以来;其矿床的形成不仅受成矿母岩、地球化学、构造等内在因素的影响,亦受地形地貌、气候和植被等外在因素的控制,在勐海回龙卡-帕宫苏胡一带形成一条北西-南东向的稀土矿富集带.结合1:5万矿调工作成果,认为勐海地区成矿地质条件优越,具有很大的离子吸附型稀土矿找矿前景.
AbstractList P618.7; 云南勐海地区地处临沧-勐海(岩浆弧)Fe-Pb-Zn-Au-Ag-Sn-Sb-Ge-REE矿带(Ⅳ9)南段,近年来该区发现多个离子吸附型稀土矿床.为查明勐海地区离子吸附型稀土矿床控矿因素,指导后续找矿工作,本文在野外地质调查和室内综合整理分析的基础上,对勐海地区离子吸附型稀土矿床的成矿地质背景和成矿特征进行了初步研究,探讨了本区离子吸附型稀土矿床控矿因素与找矿前景.研究表明,勐海地区离子吸附型稀土矿床是以轻稀土为主的稀土矿,其成矿母岩为晚三叠世临沧花岗岩,次生富集成矿于新生代以来;其矿床的形成不仅受成矿母岩、地球化学、构造等内在因素的影响,亦受地形地貌、气候和植被等外在因素的控制,在勐海回龙卡-帕宫苏胡一带形成一条北西-南东向的稀土矿富集带.结合1:5万矿调工作成果,认为勐海地区成矿地质条件优越,具有很大的离子吸附型稀土矿找矿前景.
Author 蓝信杰
张保涛
王明波
卢文姬
王禹杰
韩成
赵宪东
李星亮
AuthorAffiliation 中国冶金地质总局山东正元地质勘查院,山东济南 250101
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LAN Xinjie
LU Wenji
LI Xingliang
WANG Mingbo
ZHANG Baotao
WANG Yujie
ZHAO Xiandong
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黑云二长花岗岩
云南省
潜力评价
勐海县
离子吸附型稀土矿
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