哈萨克斯坦西部Mugodzhary山Berchogur坳陷泥盆系—石炭系界线剖面研究进展

{"title":"哈萨克斯坦西部Mugodzhary山Berchogur坳陷泥盆系—石炭系界线剖面研究进展","authors":"S. Nikolaeva, E. Kulagina, S. Mustapayeva, A. Alekseev, Y. Gatovsky, J. Denayer, V. Ohar, A. Kurilenko, Valentina Ja. Zhaimina, E. V. Mychko","doi":"10.1007/s12542-022-00611-z","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":54648,"journal":{"name":"Palz","volume":"31 1","pages":"415 - 447"},"PeriodicalIF":1.9000,"publicationDate":"2022-05-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":"{\"title\":\"Progress in the study of the Devonian–Carboniferous boundary sections in the Berchogur Depression (Mugodzhary Mountains, western Kazakhstan)\",\"authors\":\"S. Nikolaeva, E. Kulagina, S. Mustapayeva, A. Alekseev, Y. Gatovsky, J. Denayer, V. Ohar, A. Kurilenko, Valentina Ja. Zhaimina, E. V. Mychko\",\"doi\":\"10.1007/s12542-022-00611-z\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":54648,\"journal\":{\"name\":\"Palz\",\"volume\":\"31 1\",\"pages\":\"415 - 447\"},\"PeriodicalIF\":1.9000,\"publicationDate\":\"2022-05-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"4\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Palz\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1007/s12542-022-00611-z\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"PALEONTOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Palz","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1007/s12542-022-00611-z","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"PALEONTOLOGY","Score":null,"Total":0}