川西九龙黄牛坪铍矿床地质特征及找矿潜力

doi:10.19388/j.zgdzdc.2019.06.09

Abstract
Figure/Table
References
Related Citation (15)

Download: PDF (2724 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract Through the comprehensive geological survey in Sanchahe area of Jiulong, Western Sichuan, the authors found that there was a good beryllium mineralization belt near the contact zone between Qiaopengzi rock mass and Triassic surrounding rocks. Four beryllium ore bodies were initially identified in NNW direction, extending along the contact zone of the rock mass. BeO grade can reach up to 0.698%, and the preliminarily predicted BeO resources can be of large scale. The ore mineral is mainly beryl, and the main surrounding rock alteration is tourmaline alteration. The top of the granite mass is also an important metallogenic location of the pegmatite-bearing rock. Remote sensing technology was used in the field of ore prospecting to recognize anomalies, and then large-scale recourse on remote sensing anomalies were carried out. Besides, further engineering methods were used for verification. The results show that the lithium and beryllium anomalies of water sediments in Jiulong area are high, with high matching degree of regional geological conditions. On the periphery of the study area, there is Daqianggou lithium-beryllium deposit in the east, and in the south a large number of spodumene-bearing pegmatites were traced in Wulaxi area, indicating that this area has good metallogenic conditions and prospecting potential.

Key words： Huangniuping,Jiulong beryllium geological characteristic prospecting potential

Received: 13 March 2019

ZTFLH:

P618.72

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	WANG Wei
	LIU Tuqiang
	YUAN Linping
	LIU Shanbao
	YU Yang
	LIU Lijun
	LV Bingting
	ZHENG Xiaogang
	DAI Hongzhang

Cite this article:

WANG Wei,LIU Tuqiang,YUAN Linping, et al. Geological characteristics and prospecting potential of Huangniuping beryllium deposit in Jiulong of West Sichuan[J]. , 2019, 6(6): 72-78.

URL:

http://www.zgdzdcbjb.com/EN/10.19388/j.zgdzdc.2019.06.09 OR http://www.zgdzdcbjb.com/EN/Y2019/V6/I6/72

[1] 邹天人,李庆昌.中国新疆稀有及稀土金属矿床[M].北京:地质出版社,2006:1-10.
[2] 费光春,袁天晶,唐文春,等.川西可尔因伟晶岩型稀有金属矿床含矿伟晶岩分类浅析[J].矿床地质,2014,33(增刊1):187-188.
[3] 付小方,袁蔺平,王登红,等.四川甲基卡矿田新三号稀有金属矿脉的成矿特征与勘查模型[J].矿床地质,2015,34(6):1172-1186.
[4] 付小方,侯立玮,王登红,等.四川甘孜甲基卡锂辉石矿矿产调查评价成果[J].中国地质调查,2014,1(3):37-43.
[5] 古城会. 四川省可尔因伟晶岩田东南密集区锂辉石矿床成矿规律[J].地质找矿论丛,2014,29(1):59-65.
[6] 饶魁元. 四川马尔康地拉秋锂矿床地质特征及找矿方向[J].四川有色金属,2016(1):54-57.
[7] 王登红,付小方.四川甲基卡外围锂矿找矿取得突破[J].岩矿测试,2013,32(6):987.
[8] 王登红. 四川发现超大规模锂矿储量逾60万吨[J].中国有色建设,2014(3):33.
[9] 王登红,王瑞江,付小方,等.对能源金属矿产资源基地调查评价基本问题的探讨——以四川甲基卡大型锂矿基地为例[J].地球学报,2016,37(4):471-480.
[10] 王子平,刘善宝,马圣钞,等.四川阿坝州党坝超大型锂辉石矿床成矿规律及深部和外围找矿方向[J].地球科学,2018,43(6):2029-2041.
[11] 易仲康,马钰权.雅江残余盆地南北缘伟晶岩稀有金属矿地质特征[J].四川地质学报,2018,38(2):260-263,273.
[12] 王登红,唐菊兴,应立娟,等.“五层楼+地下室”找矿模型的适用性及其对深部找矿的意义[J].吉林大学学报:地球科学版,2010,40(4):733-738.
[13] 王登红,王成辉,孙艳,等.我国锂铍钽矿床调查研究进展及相关问题简述[J].中国地质调查,2017,4(5):1-8.
[14] 王登红,刘丽君,侯江龙,等.初论甲基卡式稀有金属矿床“五层楼+地下室”勘查模型[J].地学前缘,2017,24(5):1-7.
[15] 李建康,刘喜方,王登红.中国锂矿成矿规律概要[J].地质学报,2014,88(12):2269-2283.
[16] 李会正. 四川省九龙县打枪沟锂铍稀有金属矿详查报告[R].成都:四川省冶金地质勘查局水文工程大队,2013.
[17] 殷聃,张洪超,何成麟.四川省九龙县久鲁祝地区稀有金属矿勘查选区报告[R].成都:成都理工大学,2014.
[18] 殷聃. 四川省九龙县打枪沟锂铍矿床地质特征及找矿潜力研究[D].成都:成都理工大学,2017.
[19] 四川省冶金地质勘查局水文工程大队.四川省九龙县久鲁祝锂多金属矿预查报告[R].成都:四川省冶金地质勘查局水文工程大队,2013.