南岭花岗岩液体偏析实验研究

Science in China Series B-Chemistry, Biological, Agricultural, Medical & Earth Sciences Pub Date : 1988-09-10 DOI:10.1360/YB1988-31-9-1122

Wang Liankui, Lu Jialan, Zhang Shaoli, Yang Wenjin, Xue Wenxin

{"title":"南岭花岗岩液体偏析实验研究","authors":"Wang Liankui, Lu Jialan, Zhang Shaoli, Yang Wenjin, Xue Wenxin","doi":"10.1360/YB1988-31-9-1122","DOIUrl":null,"url":null,"abstract":"Based on the characteristics of granites of the Nanling region, a procedure was specially designed to do experiment on the immiscible liquid phase. The starting materials were biotite granite + NnF + LiF. Under 1000 bar and 840℃, more than two immiscible liquid phases were produced from the homogeneous granite melt rich in F and Li. Electron microprobe data suggest that the immiscible liquid phases can be divided into (ⅰ) a silicate melt rich in F and Fe (melanocratic glass balls), (ⅱ) a silicate melt poor in F (matrix glass), and (ⅲ) a melt consisting mainly of fluorates (leucocratic glass balls). In conjunction with the chemical and mineral compositions, the structure and texture of granites in the Nanling region, the experimental results are discussed in this paper. The theory of liquid immiscibility can well account for the globular structure, glass inclusions pressent in minerals mineralized globular \"inclusions\", flow structure, banded structure and layer structure as are observed in Nanling granites.","PeriodicalId":223601,"journal":{"name":"Science in China Series B-Chemistry, Biological, Agricultural, Medical & Earth Sciences","volume":"25 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1988-09-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"AN EXPERIMENTAL STUDY ON LIQUID SEGREGATION OF NANLING GRANITES\",\"authors\":\"Wang Liankui, Lu Jialan, Zhang Shaoli, Yang Wenjin, Xue Wenxin\",\"doi\":\"10.1360/YB1988-31-9-1122\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Based on the characteristics of granites of the Nanling region, a procedure was specially designed to do experiment on the immiscible liquid phase. The starting materials were biotite granite + NnF + LiF. Under 1000 bar and 840℃, more than two immiscible liquid phases were produced from the homogeneous granite melt rich in F and Li. Electron microprobe data suggest that the immiscible liquid phases can be divided into (ⅰ) a silicate melt rich in F and Fe (melanocratic glass balls), (ⅱ) a silicate melt poor in F (matrix glass), and (ⅲ) a melt consisting mainly of fluorates (leucocratic glass balls). In conjunction with the chemical and mineral compositions, the structure and texture of granites in the Nanling region, the experimental results are discussed in this paper. The theory of liquid immiscibility can well account for the globular structure, glass inclusions pressent in minerals mineralized globular \\\"inclusions\\\", flow structure, banded structure and layer structure as are observed in Nanling granites.\",\"PeriodicalId\":223601,\"journal\":{\"name\":\"Science in China Series B-Chemistry, Biological, Agricultural, Medical & Earth Sciences\",\"volume\":\"25 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1988-09-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Science in China Series B-Chemistry, Biological, Agricultural, Medical & Earth Sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1360/YB1988-31-9-1122\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Science in China Series B-Chemistry, Biological, Agricultural, Medical & Earth Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1360/YB1988-31-9-1122","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}

引用次数: 3

摘要

根据南岭地区花岗岩的特点，设计了一套不混相液相实验程序。起始物质为黑云母花岗岩+ NnF + liff。在1000 bar和840℃条件下，富F、富Li均质花岗岩熔体产生两种以上不混相。电子探针数据表明，不混溶液相可分为(ⅰ)富F和Fe的硅酸盐熔体(黑晶玻璃球)、(ⅱ)贫F的硅酸盐熔体(基质玻璃)和(ⅲ)主要由氟化物组成的熔体(白晶玻璃球)。结合南岭地区花岗岩的化学成分、矿物组成、结构和质地，对实验结果进行了讨论。液体不混溶理论可以很好地解释南岭花岗岩的球状结构、矿化球状“包裹体”中的玻璃包裹体、流状结构、带状结构和层状结构。

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

AN EXPERIMENTAL STUDY ON LIQUID SEGREGATION OF NANLING GRANITES

Based on the characteristics of granites of the Nanling region, a procedure was specially designed to do experiment on the immiscible liquid phase. The starting materials were biotite granite + NnF + LiF. Under 1000 bar and 840℃, more than two immiscible liquid phases were produced from the homogeneous granite melt rich in F and Li. Electron microprobe data suggest that the immiscible liquid phases can be divided into (ⅰ) a silicate melt rich in F and Fe (melanocratic glass balls), (ⅱ) a silicate melt poor in F (matrix glass), and (ⅲ) a melt consisting mainly of fluorates (leucocratic glass balls). In conjunction with the chemical and mineral compositions, the structure and texture of granites in the Nanling region, the experimental results are discussed in this paper. The theory of liquid immiscibility can well account for the globular structure, glass inclusions pressent in minerals mineralized globular "inclusions", flow structure, banded structure and layer structure as are observed in Nanling granites.

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

Science in China Series B-Chemistry, Biological, Agricultural, Medical & Earth Sciences

自引率

0.00%

发文量