辽东—吉南地区下元古界硼矿床成因的商榷——兼论容矿大理岩及硼矿矿床的成因
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摘要
辽东—吉南地区下元古界产有丰富的硼矿资源,半个多世纪以来几乎所有硼矿地质勘查报告及有关论文、专著等无不涉及矿床成因。关于硼矿床成因主要有沉积变质成矿、沉积变质再造成矿、超变质热液成矿等3种观点(称传统观点,下同),传统观点认为硼的成矿物质来源于下元古界地层,经混合岩化或超变质热液将地层中分散的硼活化、迁移至镁质大理岩富集成矿。在编纂《中国矿产地质志·硼矿卷》过程中,对辽吉硼矿进行了新一轮研究,认为传统观点硼矿床成因值得商榷,并提出碳酸岩岩浆期后含硼热液交代早期喷溢的碳酸岩成矿的论说。
There are lots of boron resources in Lower Proterozoic Erathem of eastern Liaoning and southern Jilin. For more than half a century, almost all of geological survey reports, papers and monographs on boron deposits involve genesis of deposits. There are 3 kinds of traditional views of genesis of boron deposits: sedimento-metamorphic deposit, sedimento-metamorphic–remoulded deposit and ultrametamorphism-hydrothermal deposit. From traditional views, we can summarize that metallogenic materials are from Lower Proterozoic Erathem, and the dispersed boron in stratum is activated and migrated into magnesia marble to enrich by these materials which are are subjected to migmatization or ultrametamorphism. In the compilation of "Volume for Boron of Mineral Geology of China", boron deposits in Liaoning and Jilin are further studied. We consider that it is worth discussed for the traditional genesis of boron, and based on the study, we carry out a new argument that hydrothermal containing boron metasomatics early eruption carbonate rocks to mineralization after the magmatic period of carbonatite.
There are lots of boron resources in Lower Proterozoic Erathem of eastern Liaoning and southern Jilin. For more than half a century, almost all of geological survey reports, papers and monographs on boron deposits involve genesis of deposits. There are 3 kinds of traditional views of genesis of boron deposits: sedimento-metamorphic deposit, sedimento-metamorphic–remoulded deposit and ultrametamorphism-hydrothermal deposit. From traditional views, we can summarize that metallogenic materials are from Lower Proterozoic Erathem, and the dispersed boron in stratum is activated and migrated into magnesia marble to enrich by these materials which are are subjected to migmatization or ultrametamorphism. In the compilation of "Volume for Boron of Mineral Geology of China", boron deposits in Liaoning and Jilin are further studied. We consider that it is worth discussed for the traditional genesis of boron, and based on the study, we carry out a new argument that hydrothermal containing boron metasomatics early eruption carbonate rocks to mineralization after the magmatic period of carbonatite.
引文
1王秀璋.东北内生硼矿床的矿物组成和矿床成因研究[M].北京:科学出版社,1974
2张秋生.中国早前寒武纪地质及成矿作用[M].长春:吉林人民出版社,1984
3姜春潮,等.辽吉东部前寒武纪地质[M].沈阳:辽宁科学技术出版社,1987
4姜春潮,刘光启.宽甸群中的层控矿床[J].矿床地质,1983(3):1~7
5《中国矿床》编委会编.中国矿床(下册)[M],北京:地质出版社,1994.
6冯本智,卢静文,邹日,等.中国辽吉地区早元古代大型-超大型硼矿床的形成条件[J].长春科技大学学术报,1998,28(1):1~15
7邹日.营口虎皮峪地区早元古代含硼岩系中热水沉积建造特征及硼矿床成因[D].长春:长春地质学院,1993
8《中国化工矿产地质概论》编写组编.中国化工矿产地质概论[R].涿州:化工矿产地质研究院,2001,138~193
9刘敬党,肖荣阁.辽东硼矿区域成矿模型[M].北京:地质出版社,2007
10李雪梅.辽东-吉南硼矿带硼矿成矿作用及成矿远景评价[D].长春:吉林大学,2009
11陈毓川,熊先孝,等.中国硼矿成矿规律[M].北京:地质出版社,2014
12韩豫川,熊先孝,孙小虹,等.中国硼矿成矿规律[M].北京:地质出版社,2014
13黄作良,莫珉,祖恩东.辽东硼矿床中电气石的矿物学特征及成因意义[J].岩石矿物学杂志,1996,15(4):365~378
14程裕淇.中国区域地质概念[M].北京:地质出版社,1994
15辽宁省地质矿产调查院,辽宁省硼矿资源潜力评价成果报告[R].沈阳:辽宁省地质矿产地质调查院,2012
16东野脉兴,熊先孝,栾俊霞,等.辽东-吉南地区下元古界含硼岩系的厘定[J].化工矿产地质,2017,39(4)
17武汉地质学院岩石教研室编.岩浆岩岩石学(上)[M].武汉:中国地质大学出版社,1980
18白鸽,袁忠信.碳酸岩地质及矿产[M].中国地质科学院矿床地质研究所所刊第1号(总第13号).北京:地质出版社,1985
19东野脉兴.世界内生磷矿地质及成矿规律[J].化工矿产地质,2004,26(3):134~144
20熊先孝,肖荣阁,刘长学.辽东吉南地区富镁大理岩的成因及找矿意义[J].化工矿物与加工,2010(1):23~26
21胡墨田,王培君.辽东-吉南地区硼矿床地质特征及成矿规律[J].化工矿产地质,1993,15(3):161~168
2张秋生.中国早前寒武纪地质及成矿作用[M].长春:吉林人民出版社,1984
3姜春潮,等.辽吉东部前寒武纪地质[M].沈阳:辽宁科学技术出版社,1987
4姜春潮,刘光启.宽甸群中的层控矿床[J].矿床地质,1983(3):1~7
5《中国矿床》编委会编.中国矿床(下册)[M],北京:地质出版社,1994.
6冯本智,卢静文,邹日,等.中国辽吉地区早元古代大型-超大型硼矿床的形成条件[J].长春科技大学学术报,1998,28(1):1~15
7邹日.营口虎皮峪地区早元古代含硼岩系中热水沉积建造特征及硼矿床成因[D].长春:长春地质学院,1993
8《中国化工矿产地质概论》编写组编.中国化工矿产地质概论[R].涿州:化工矿产地质研究院,2001,138~193
9刘敬党,肖荣阁.辽东硼矿区域成矿模型[M].北京:地质出版社,2007
10李雪梅.辽东-吉南硼矿带硼矿成矿作用及成矿远景评价[D].长春:吉林大学,2009
11陈毓川,熊先孝,等.中国硼矿成矿规律[M].北京:地质出版社,2014
12韩豫川,熊先孝,孙小虹,等.中国硼矿成矿规律[M].北京:地质出版社,2014
13黄作良,莫珉,祖恩东.辽东硼矿床中电气石的矿物学特征及成因意义[J].岩石矿物学杂志,1996,15(4):365~378
14程裕淇.中国区域地质概念[M].北京:地质出版社,1994
15辽宁省地质矿产调查院,辽宁省硼矿资源潜力评价成果报告[R].沈阳:辽宁省地质矿产地质调查院,2012
16东野脉兴,熊先孝,栾俊霞,等.辽东-吉南地区下元古界含硼岩系的厘定[J].化工矿产地质,2017,39(4)
17武汉地质学院岩石教研室编.岩浆岩岩石学(上)[M].武汉:中国地质大学出版社,1980
18白鸽,袁忠信.碳酸岩地质及矿产[M].中国地质科学院矿床地质研究所所刊第1号(总第13号).北京:地质出版社,1985
19东野脉兴.世界内生磷矿地质及成矿规律[J].化工矿产地质,2004,26(3):134~144
20熊先孝,肖荣阁,刘长学.辽东吉南地区富镁大理岩的成因及找矿意义[J].化工矿物与加工,2010(1):23~26
21胡墨田,王培君.辽东-吉南地区硼矿床地质特征及成矿规律[J].化工矿产地质,1993,15(3):161~168