Drona Adhikari, Keshav Shrestha, Purushottam Adhikari, K. Paudayal, L. Paudel
{"title":"尼泊尔东部Sunsari-Udayapur地区Chatara-Barahakshetra剖面地质研究","authors":"Drona Adhikari, Keshav Shrestha, Purushottam Adhikari, K. Paudayal, L. Paudel","doi":"10.3126/BDG.V20I0.20723","DOIUrl":null,"url":null,"abstract":"Geological mapping was carried out in the Chatara–Barahakshetra area of east Nepal. The Siwalik of the Chatara–Barahakshetra area is divided into the Lower Siwalik and the Middle Siwalik. Each unit is further subdivided into lower and upper members. The Central Churia Thrust is overturned in the study area. Highly deformed Siwalik contain several outcrop-scale as well as a large-scale folds. Bulletin of Department of Geology, vol. 20-21, 2018, pp: 49-58","PeriodicalId":356325,"journal":{"name":"Bulletin of The Department of Geology","volume":"2140 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-08-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"Geological Study of Chatara–Barahakshetra Section, Sunsari-Udayapur District, Eastern Nepal\",\"authors\":\"Drona Adhikari, Keshav Shrestha, Purushottam Adhikari, K. Paudayal, L. Paudel\",\"doi\":\"10.3126/BDG.V20I0.20723\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Geological mapping was carried out in the Chatara–Barahakshetra area of east Nepal. The Siwalik of the Chatara–Barahakshetra area is divided into the Lower Siwalik and the Middle Siwalik. Each unit is further subdivided into lower and upper members. The Central Churia Thrust is overturned in the study area. Highly deformed Siwalik contain several outcrop-scale as well as a large-scale folds. Bulletin of Department of Geology, vol. 20-21, 2018, pp: 49-58\",\"PeriodicalId\":356325,\"journal\":{\"name\":\"Bulletin of The Department of Geology\",\"volume\":\"2140 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2018-08-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Bulletin of The Department of Geology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.3126/BDG.V20I0.20723\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of The Department of Geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3126/BDG.V20I0.20723","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Geological Study of Chatara–Barahakshetra Section, Sunsari-Udayapur District, Eastern Nepal
Geological mapping was carried out in the Chatara–Barahakshetra area of east Nepal. The Siwalik of the Chatara–Barahakshetra area is divided into the Lower Siwalik and the Middle Siwalik. Each unit is further subdivided into lower and upper members. The Central Churia Thrust is overturned in the study area. Highly deformed Siwalik contain several outcrop-scale as well as a large-scale folds. Bulletin of Department of Geology, vol. 20-21, 2018, pp: 49-58
京公网安备 11010802042870号
京ICP备2023020795号-1
分享
求助内容：
应助结果提醒方式：
扫码关注我们
