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,{"id":71362,"text":"tei314 - 1953 - A mineralogic study of churn drill cuttings from a well through the Bone Valley formation, Hillsborough County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"tei314","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"314","title":"A mineralogic study of churn drill cuttings from a well through the Bone Valley formation, Hillsborough County, Florida","language":"ENGLISH","doi":"10.3133/tei314","usgsCitation":"Berman, R., 1953, A mineralogic study of churn drill cuttings from a well through the Bone Valley formation, Hillsborough County, Florida: U.S. Geological Survey Trace Elements Investigations 314, 20 p., https://doi.org/10.3133/tei314.","productDescription":"20 p.","costCenters":[],"links":[{"id":193332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/314/report-thumb.jpg"},{"id":90693,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/314/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adfd8","contributors":{"authors":[{"text":"Berman, Robert","contributorId":13315,"corporation":false,"usgs":true,"family":"Berman","given":"Robert","affiliations":[],"preferred":false,"id":284052,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13627,"text":"ofr5371 - 1953 - Stratigraphic relations of the Shakopee dolomite and the St. Peter sandstone in southwestern Wisconsin","interactions":[{"subject":{"id":13627,"text":"ofr5371 - 1953 - Stratigraphic relations of the Shakopee dolomite and the St. Peter sandstone in southwestern Wisconsin","indexId":"ofr5371","publicationYear":"1953","noYear":false,"title":"Stratigraphic relations of the Shakopee dolomite and the St. Peter sandstone in southwestern Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":39134,"text":"pp274K - 1956 - Stratigraphy of Middle Ordovician rocks in the zinc-lead district of Wisconsin, Illinois, and Iowa","indexId":"pp274K","publicationYear":"1956","noYear":false,"chapter":"K","title":"Stratigraphy of Middle Ordovician rocks in the zinc-lead district of Wisconsin, Illinois, and Iowa"},"id":1}],"supersededBy":{"id":39134,"text":"pp274K - 1956 - Stratigraphy of Middle Ordovician rocks in the zinc-lead district of Wisconsin, Illinois, and Iowa","indexId":"pp274K","publicationYear":"1956","noYear":false,"title":"Stratigraphy of Middle Ordovician rocks in the zinc-lead district of Wisconsin, Illinois, and Iowa"},"lastModifiedDate":"2025-05-29T15:29:52.003884","indexId":"ofr5371","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"53-71","title":"Stratigraphic relations of the Shakopee dolomite and the St. Peter sandstone in southwestern Wisconsin","docAbstract":"<p>This paper is concerned with the origin and geologic history of the boundary that separates the widespread St. Peter sandstone from the underlying Shakopee dolomite. That international surface is highly undulatory, and most contemporary geologists who have examined it believe that the contact irregularities result from pre-St. Peter subaerial erosion of the upper Shakopee surface. Some earlier investigators do not entirely concur.</p><p>This report is a by-product of work done for the U. S. Geological Survey during an investigation of the lead-zinc resources of Wisconsin by the U. S. Geological Survey in cooperation with the Wisconsin Geological and Natural History Survey. Attention was focused on the problem by stratigraphic studies of the Prairie du Chien formations, particularly of the Shakopee dolomite, in which structural and lithologic characters observed in the carbonate sediments seemed to be incompatible with the widely accepted erosional origin of the upper Shakopee surface. It was decided, in 1950, to explore the whole problem of the Shakopee-St. Peter relations by detailed outcrop examinations, supplemented by subsurface and other studies that might contribute to a better understanding of the genetic relationships involved. The area of the investigation was restricted to three counties in southwestern Wisconsin and closely adjacent areas in Iowa(fig. 1), differing in this respect from the broader and more general studies that previously have tended to be the rule.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5371","collaboration":"Prepared in cooperation with the Wisconsin Geological and Natural History Survey","usgsCitation":"Flint, A.E., 1953, Stratigraphic relations of the Shakopee dolomite and the St. Peter sandstone in southwestern Wisconsin: U.S. Geological Survey Open-File Report 53-71, Report: vii, 129 p.; 1 Figure: 40.29 x 29.07 inches, https://doi.org/10.3133/ofr5371.","productDescription":"Report: vii, 129 p.; 1 Figure: 40.29 x 29.07 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