{"title":"基于 XRF 地球化学数据的北戈隆塔洛地区多洛卡帕地层砂岩的成因分析","authors":"Nengah Sandi, Aang Panji, Permana, Muhammad Kasim","doi":"10.20527/es.v20i1.18843","DOIUrl":null,"url":null,"abstract":"The research location is located in Deme 1 Village, East Sumalata District, North Gorontalo Regency. The rock outcrops studied are sandstones which are part of the Dolokapa Formation which is spread in the northern part of the Tilamuta Sheet. This study aims to analyze the tectonic setting of the origin of the sandstones. The research method used to achieve the research objectives is using two methods consisting of field geological surveys and X-Ray Fluoresence (XRF) Geochemical laboratory analysis. Based on the results and discussion that the two sandstone samples are of the Fe-Shale and Fe-Sand types which originate from the ARC (oceanic island arc) tectonic setting.","PeriodicalId":512914,"journal":{"name":"EnviroScienteae","volume":"71 6","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-03-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"ANALISIS PROVENANCE BATUPASIR FORMASI DOLOKAPA KABUPATEN GORONTALO UTARA BERDASARKAN DATA GEOKIMIA XRF\",\"authors\":\"Nengah Sandi, Aang Panji, Permana, Muhammad Kasim\",\"doi\":\"10.20527/es.v20i1.18843\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The research location is located in Deme 1 Village, East Sumalata District, North Gorontalo Regency. The rock outcrops studied are sandstones which are part of the Dolokapa Formation which is spread in the northern part of the Tilamuta Sheet. This study aims to analyze the tectonic setting of the origin of the sandstones. The research method used to achieve the research objectives is using two methods consisting of field geological surveys and X-Ray Fluoresence (XRF) Geochemical laboratory analysis. Based on the results and discussion that the two sandstone samples are of the Fe-Shale and Fe-Sand types which originate from the ARC (oceanic island arc) tectonic setting.\",\"PeriodicalId\":512914,\"journal\":{\"name\":\"EnviroScienteae\",\"volume\":\"71 6\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-03-04\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"EnviroScienteae\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.20527/es.v20i1.18843\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"EnviroScienteae","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.20527/es.v20i1.18843","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
研究地点位于北哥伦塔罗省东苏马拉塔区德梅 1 村。所研究的岩石露头为砂岩，属于多洛卡帕岩层（Dolokapa Formation）的一部分，该岩层分布在蒂拉姆塔岩层（Tilamuta Sheet）的北部。本研究旨在分析砂岩起源的构造环境。为实现研究目标，采用了野外地质调查和 X 射线荧光地球化学实验室分析两种研究方法。根据结果和讨论，这两个砂岩样本属于铁-页岩和铁-砂岩类型，源自 ARC（大洋岛弧）构造环境。
ANALISIS PROVENANCE BATUPASIR FORMASI DOLOKAPA KABUPATEN GORONTALO UTARA BERDASARKAN DATA GEOKIMIA XRF
The research location is located in Deme 1 Village, East Sumalata District, North Gorontalo Regency. The rock outcrops studied are sandstones which are part of the Dolokapa Formation which is spread in the northern part of the Tilamuta Sheet. This study aims to analyze the tectonic setting of the origin of the sandstones. The research method used to achieve the research objectives is using two methods consisting of field geological surveys and X-Ray Fluoresence (XRF) Geochemical laboratory analysis. Based on the results and discussion that the two sandstone samples are of the Fe-Shale and Fe-Sand types which originate from the ARC (oceanic island arc) tectonic setting.
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