{"title":"匈牙利南部Mecsek山的上石炭世植物区系","authors":"Csaba Gulyás-Kis","doi":"10.1556/AGEOL.46.2003.1.8","DOIUrl":null,"url":null,"abstract":"Upper Carboniferous pebbles are known from Miocene conglomerates (Szaszvar Formation) in the Mecsek Mts. Some pebbles may contain floral elements. Fine-grained siltstone is the most common fossiliferous rock. There are known leaf and stem fragments and some silicified wood-trunk fragments. These floral elements show Namurian to late Westphalian ages, but primarily the Westphalian B and C. The floral elements could be related to the Polish Carboniferous flora, particularly that of Silesia.","PeriodicalId":107929,"journal":{"name":"Acta Geologica Hungarica","volume":"91 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2003-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"5","resultStr":"{\"title\":\"Upper Carboniferous flora from the Mecsek Mts (Southern Hungary) - summarized results\",\"authors\":\"Csaba Gulyás-Kis\",\"doi\":\"10.1556/AGEOL.46.2003.1.8\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Upper Carboniferous pebbles are known from Miocene conglomerates (Szaszvar Formation) in the Mecsek Mts. Some pebbles may contain floral elements. Fine-grained siltstone is the most common fossiliferous rock. There are known leaf and stem fragments and some silicified wood-trunk fragments. These floral elements show Namurian to late Westphalian ages, but primarily the Westphalian B and C. The floral elements could be related to the Polish Carboniferous flora, particularly that of Silesia.\",\"PeriodicalId\":107929,\"journal\":{\"name\":\"Acta Geologica Hungarica\",\"volume\":\"91 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2003-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"5\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Acta Geologica Hungarica\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1556/AGEOL.46.2003.1.8\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Acta Geologica Hungarica","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1556/AGEOL.46.2003.1.8","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Upper Carboniferous flora from the Mecsek Mts (Southern Hungary) - summarized results
Upper Carboniferous pebbles are known from Miocene conglomerates (Szaszvar Formation) in the Mecsek Mts. Some pebbles may contain floral elements. Fine-grained siltstone is the most common fossiliferous rock. There are known leaf and stem fragments and some silicified wood-trunk fragments. These floral elements show Namurian to late Westphalian ages, but primarily the Westphalian B and C. The floral elements could be related to the Polish Carboniferous flora, particularly that of Silesia.
求助内容：
应助结果提醒方式：
京公网安备 11010802042870号
