{"title":"犹他州凯恩县煤炭中石化木材的赋存","authors":"H. Doelling","doi":"10.34191/ug-4-1_29","DOIUrl":null,"url":null,"abstract":"Silicified wood has been found in a thin coal bed of the Dakota Formation (lowest Upper Cretaceous) in the southwestern Kaiparowits Plateau in Kane County, Utah. It is not expected that metamorphic processes would partly coalify and partly silicify the plant remains. The occurrence is local. No significant coarse clastic material, other than the logs, is present in the coal bed. No satisfactory explanation for its presence can be deduced.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"6 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Occurrence of Petrified Wood in Coal, Kane County, Utah\",\"authors\":\"H. Doelling\",\"doi\":\"10.34191/ug-4-1_29\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Silicified wood has been found in a thin coal bed of the Dakota Formation (lowest Upper Cretaceous) in the southwestern Kaiparowits Plateau in Kane County, Utah. It is not expected that metamorphic processes would partly coalify and partly silicify the plant remains. The occurrence is local. No significant coarse clastic material, other than the logs, is present in the coal bed. No satisfactory explanation for its presence can be deduced.\",\"PeriodicalId\":398645,\"journal\":{\"name\":\"Utah Geology\",\"volume\":\"6 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Utah Geology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.34191/ug-4-1_29\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Utah Geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.34191/ug-4-1_29","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Occurrence of Petrified Wood in Coal, Kane County, Utah
Silicified wood has been found in a thin coal bed of the Dakota Formation (lowest Upper Cretaceous) in the southwestern Kaiparowits Plateau in Kane County, Utah. It is not expected that metamorphic processes would partly coalify and partly silicify the plant remains. The occurrence is local. No significant coarse clastic material, other than the logs, is present in the coal bed. No satisfactory explanation for its presence can be deduced.
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