矿岩浆在矿床形成中的作用

Q4 Earth and Planetary Sciences

Geology and Mineral Resources of Siberia Pub Date : 2021-01-01 DOI:10.20403/2078-0575-2021-2-84-91

S. S. Dolgushin, A. P. Dolgushin, Berezovgeologia

{"title":"矿岩浆在矿床形成中的作用","authors":"S. S. Dolgushin, A. P. Dolgushin, Berezovgeologia","doi":"10.20403/2078-0575-2021-2-84-91","DOIUrl":null,"url":null,"abstract":"Notions are substantiated that for a certain group of so-called hydrothermal deposits, not regular lowconcentration hydrothermal solutions, including their more concentrated derivatives, colloids, are not of decisive importance in their formation, but highly concentrated magmatic systems – ore magmas forming deposits by intrusive way, at a time when hydrothermal (including gas-hydrothermal) solutions coexisting with them, being more mobile and chemically active, produce only metasomatic changes in the host rocks and wallrock dissemination, masking the magmatic nature of deposits.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":"1 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"ROLE OF ORE MAGMAS IN THE FORMATION OF DEPOSITS\",\"authors\":\"S. S. Dolgushin, A. P. Dolgushin, Berezovgeologia\",\"doi\":\"10.20403/2078-0575-2021-2-84-91\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Notions are substantiated that for a certain group of so-called hydrothermal deposits, not regular lowconcentration hydrothermal solutions, including their more concentrated derivatives, colloids, are not of decisive importance in their formation, but highly concentrated magmatic systems – ore magmas forming deposits by intrusive way, at a time when hydrothermal (including gas-hydrothermal) solutions coexisting with them, being more mobile and chemically active, produce only metasomatic changes in the host rocks and wallrock dissemination, masking the magmatic nature of deposits.\",\"PeriodicalId\":52268,\"journal\":{\"name\":\"Geology and Mineral Resources of Siberia\",\"volume\":\"1 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geology and Mineral Resources of Siberia\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.20403/2078-0575-2021-2-84-91\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"Earth and Planetary Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geology and Mineral Resources of Siberia","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.20403/2078-0575-2021-2-84-91","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}

引用次数: 0

摘要

证实了这样的观点，即对于某一类所谓的热液矿床，不是规则的低浓度热液，包括其更浓缩的衍生物，胶体，在其形成过程中起决定性作用，而是高度浓缩的岩浆系统，即矿岩浆通过侵入方式形成矿床，此时热液(包括气热液)溶液与之共存，更具流动性和化学活性。仅在寄主岩和围岩中产生交代变化，掩盖了矿床的岩浆性质。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

查看原文本刊更多论文

ROLE OF ORE MAGMAS IN THE FORMATION OF DEPOSITS

Notions are substantiated that for a certain group of so-called hydrothermal deposits, not regular lowconcentration hydrothermal solutions, including their more concentrated derivatives, colloids, are not of decisive importance in their formation, but highly concentrated magmatic systems – ore magmas forming deposits by intrusive way, at a time when hydrothermal (including gas-hydrothermal) solutions coexisting with them, being more mobile and chemically active, produce only metasomatic changes in the host rocks and wallrock dissemination, masking the magmatic nature of deposits.

求助全文

通过发布文献求助，成功后即可免费获取论文全文。去求助

来源期刊

Geology and Mineral Resources of Siberia Earth and Planetary Sciences-Geology

CiteScore

0.30

自引率

0.00%

发文量