Name: mtsimon_012a_temp_22

Display Field: well_name

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Description: <DIV STYLE="text-align:Left;"><DIV><DIV><P STYLE="text-align:Justify;"><SPAN>According to Sass and others (1998) and Vugrinovich (personal communication, 2000), temperature measurements of the Mt. Simon are very scarce. Therefore, we have used the generally accepted temperature gradient for the Michigan Basin, 25 °C / km (Cercone, 1984). We also have used one data point obtained from Vugrinovich (personal communication, 2000).</SPAN></P><P STYLE="text-align:Justify;"><SPAN><SPAN /></SPAN></P><P /><P><SPAN /></P></DIV></DIV></DIV>

Service Item Id: d45321a916094abe8f4775e110c4828a

Copyright Text: Cercone, K. R., 1984, Thermal history of the Michigan Basin: American Association of Petroleum Geologists Bulletin, v. 68, no. 2, p. 130–136. Vugrinovich, Raymond, 1986, Patterns of regional subsurface fluid movement in the Michigan Basin: Michigan Department of Natural Resources, Geological Survey Division, Open File Report 86-6. Vugrinovich, Raymond, 2000, Senior Geologist, Michigan Department of Environmental Quality, Geological Survey Division, personal communication.

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Spatial Reference: 102100  (3857)

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Type ID Field: null

Fields:

• objectid ( type: esriFieldTypeOID, alias: OBJECTID )
• well_name ( type: esriFieldTypeString, alias: WELL_NAME, length: 12 )
• location ( type: esriFieldTypeString, alias: LOCATION, length: 19 )
• permit ( type: esriFieldTypeInteger, alias: PERMIT )
• state ( type: esriFieldTypeString, alias: STATE, length: 7 )
• elevmasl ( type: esriFieldTypeDouble, alias: ELEVMASL )
• depth_m_ ( type: esriFieldTypeDouble, alias: DEPTH_M_ )
• tempera_c_ ( type: esriFieldTypeDouble, alias: TEMPERA_C_ )
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