黑龙江林口西北楞石墨矿地质特征及成矿规律
|
摘要
黑龙江林口西北楞石墨矿位于佳木斯—兴凯(地块)Fe-Au-P-石墨-矽线石成矿带(Ⅲ-53)中部,为一沉积变质超大型晶质石墨矿床。赋矿层位为上元古界兴东岩群大盘道岩组下段(Pt_3dp~1.),构造较为简单,矿带延展长度约为9.5 km,共圈定石墨矿带6条、石墨矿体73条。矿床地质特征及地球物理特征明显,极具代表性,总结研究其地质特征及成矿规律,对黑龙江东部佳木斯隆起兴东岩群大盘道岩组的区域矿产勘查工作具有一定的参考价值。
The Xibeileng graphite deposit in Linkou County is located in the middle of the Jiamusi-Xingkai(block) Fe-Au-P-graphite-silimanite metallogenic belt(III-53). It is a super-large sedimentary metamorphic crystalline graphite deposit, and is hosted in the lower member of the Dapandao Rock Formation(Pt_3dp~1.) of the Neoproterozoic Xingdong Rock Group. This deposit has relatively simple structures, with an extension length of ore belt at about 9.5 km, and six ore belts and 73 graphite orebodies have been delineated. The geological and geophysical characteristics of the deposit are obvious and quite typical. To summarize and study its geological characteristics and metallogenic regularities has guiding significance for regional mineral exploration of the Dapandao Rock Formation of Xingdong Rock Group in the Jiamusi Uplift of eastern Heilongjiang Province.
The Xibeileng graphite deposit in Linkou County is located in the middle of the Jiamusi-Xingkai(block) Fe-Au-P-graphite-silimanite metallogenic belt(III-53). It is a super-large sedimentary metamorphic crystalline graphite deposit, and is hosted in the lower member of the Dapandao Rock Formation(Pt_3dp~1.) of the Neoproterozoic Xingdong Rock Group. This deposit has relatively simple structures, with an extension length of ore belt at about 9.5 km, and six ore belts and 73 graphite orebodies have been delineated. The geological and geophysical characteristics of the deposit are obvious and quite typical. To summarize and study its geological characteristics and metallogenic regularities has guiding significance for regional mineral exploration of the Dapandao Rock Formation of Xingdong Rock Group in the Jiamusi Uplift of eastern Heilongjiang Province.
引文
白云峰,秦杰,孟欣,2018.我国石墨产业发展现状及需求分析[J].建材发展导向,16(20):16-18.
李超,王登红,赵鸿,等,2015.中国石墨矿床成矿规律概要[J].矿床地质,34(6):1223-1236.
李思远,孙莉,孟凡磊,等,2016.黑龙江云山石墨矿床资源潜力预测[J].地质学刊,40(2):288-292.
唐臣,2016.黑龙江石墨矿资源潜力预测[J].地质学刊,40(3):438-442.
王力,樊俊雷,李雷,等,2017.中国石墨资源概况及晶质石墨成矿规律[J].地质学刊,41(2):310-317.
王丹,孙映祥,2018.我国石墨资源勘查开发规划布局分析[J].矿产保护与利用(5):14-19.
文立坤,翟艳超,2018.黑龙江省石墨矿成矿规律分析[J].能源与环保,40(10):118-120,126.
文立坤,翟艳超,2018.佳木斯隆起孔兹岩系中石墨矿地质特征及找矿方向浅析[J].中国金属通报 (3):143-144.
徐衍强,韩振新,徐爱民,2001.佳木斯地块大型晶质石墨矿集区的形成和演化[J].黑龙江地质,12(3):1-10.
颜玲亚,高树学,孙莉,等,2018.我国区域变质型石墨矿成矿特征及成矿要素[J].中国非金属矿工业导刊(3):21-24,28.
张苏江,崔立伟,张彦文,等,2018.国内外石墨矿产资源及其分布概述[J].中国矿业,27(10):8-14.
李超,王登红,赵鸿,等,2015.中国石墨矿床成矿规律概要[J].矿床地质,34(6):1223-1236.
李思远,孙莉,孟凡磊,等,2016.黑龙江云山石墨矿床资源潜力预测[J].地质学刊,40(2):288-292.
唐臣,2016.黑龙江石墨矿资源潜力预测[J].地质学刊,40(3):438-442.
王力,樊俊雷,李雷,等,2017.中国石墨资源概况及晶质石墨成矿规律[J].地质学刊,41(2):310-317.
王丹,孙映祥,2018.我国石墨资源勘查开发规划布局分析[J].矿产保护与利用(5):14-19.
文立坤,翟艳超,2018.黑龙江省石墨矿成矿规律分析[J].能源与环保,40(10):118-120,126.
文立坤,翟艳超,2018.佳木斯隆起孔兹岩系中石墨矿地质特征及找矿方向浅析[J].中国金属通报 (3):143-144.
徐衍强,韩振新,徐爱民,2001.佳木斯地块大型晶质石墨矿集区的形成和演化[J].黑龙江地质,12(3):1-10.
颜玲亚,高树学,孙莉,等,2018.我国区域变质型石墨矿成矿特征及成矿要素[J].中国非金属矿工业导刊(3):21-24,28.
张苏江,崔立伟,张彦文,等,2018.国内外石墨矿产资源及其分布概述[J].中国矿业,27(10):8-14.