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Layer: stpeter_006_cont_sandbody_fault (71)

Name: stpeter_006_cont_sandbody_fault

Display Field: source_organization

Type: Feature Layer

Geometry Type: esriGeometryPolyline

Description: Several authors indicated that the sands within the St. Peter Sandstone are continuous, especially in the middle portions of the unit (Kreutzfeld, 1982; Barnes and others, 1992). The St. Peter Sandstone is partially offset by a number of faults, and these faults can significantly affect sand-body continuity. Therefore, we chose to use the map of Collinson and others (1988), which shows the locations of major faults that offset the St. Peter Sandstone to characterize sand-body continuity, because faulting rather than lithology is the principal factor influencing sand-body continuity of the St. Peter in the central Illinois Basin.

Service Item Id: 09f320b60acc40759527595468c9a476

Copyright Text: Collinson, C., Sargent, M. L., and Jennings, J. R., 1988, Chapter 14: Illinois Basin region, in Sloss, L. L., ed., The Geology of North America, v. D-2, Sedimentary Cover—North American Craton: U.S.: Decade of North American Geology: Geological Society of America, p. 383–426.

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Supported Query Formats: JSON, geoJSON, PBF

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Supports Advanced Queries: true

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Has Labels: false

Can Modify Layer: true

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Spatial Reference: 102100  (3857)  LatestVCSWkid(0)



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Type ID Field: null

Fields:
• objectid ( type: esriFieldTypeOID, alias: OBJECTID )
• seg_id ( type: esriFieldTypeInteger, alias: SEG_ID )
• shape_leng ( type: esriFieldTypeDouble, alias: Shape_Leng )
• source_organization ( type: esriFieldTypeString, alias: Source Organization, length: 255 )
• hyperlink ( type: esriFieldTypeString, alias: Link, length: 255 )
• resource_date ( type: esriFieldTypeString, alias: Date of Resource, length: 255 )
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