Author: Craig D. Morgan
Publisher: Utah Geological Survey
ISBN: 155791690X
Category : Technology & Engineering
Languages : en
Pages : 105
Book Description
Hydrocarbon production in the Bluebell field is from three reservoirs in the Tertiary-aged Colton and Green River Formations: (1) overpressured Colton/Flagstaff, (2) lower Green River, and (3) upper Green River. Kerogen-rich shale and marlstone deposited in marginal and nearshore openlacustrine environments are the source of the waxy crude in the Colton/Flagstaff and lower Green River. Marlstone, or oil shale and possibly coal, are the sources for the asphaltic crude found in the upper Green River. Non-associated gas in the upper Green River could be from coaly deposits in the upper Green River, or migrated up from the lower Green River, or a combination of both. The lithology of all three reservoirs is similar; fractured sandstone, shale, limestone, and marlstone beds having generally low intergranular porosity and permeability. The strata were deposited in lacustrine and alluvial environments.
The Bluebell Oil Field, Uinta Basin, Duchesne and Uintah Counties, Utah
Author: Craig D. Morgan
Publisher: Utah Geological Survey
ISBN: 155791690X
Category : Technology & Engineering
Languages : en
Pages : 105
Book Description
Hydrocarbon production in the Bluebell field is from three reservoirs in the Tertiary-aged Colton and Green River Formations: (1) overpressured Colton/Flagstaff, (2) lower Green River, and (3) upper Green River. Kerogen-rich shale and marlstone deposited in marginal and nearshore openlacustrine environments are the source of the waxy crude in the Colton/Flagstaff and lower Green River. Marlstone, or oil shale and possibly coal, are the sources for the asphaltic crude found in the upper Green River. Non-associated gas in the upper Green River could be from coaly deposits in the upper Green River, or migrated up from the lower Green River, or a combination of both. The lithology of all three reservoirs is similar; fractured sandstone, shale, limestone, and marlstone beds having generally low intergranular porosity and permeability. The strata were deposited in lacustrine and alluvial environments.
Publisher: Utah Geological Survey
ISBN: 155791690X
Category : Technology & Engineering
Languages : en
Pages : 105
Book Description
Hydrocarbon production in the Bluebell field is from three reservoirs in the Tertiary-aged Colton and Green River Formations: (1) overpressured Colton/Flagstaff, (2) lower Green River, and (3) upper Green River. Kerogen-rich shale and marlstone deposited in marginal and nearshore openlacustrine environments are the source of the waxy crude in the Colton/Flagstaff and lower Green River. Marlstone, or oil shale and possibly coal, are the sources for the asphaltic crude found in the upper Green River. Non-associated gas in the upper Green River could be from coaly deposits in the upper Green River, or migrated up from the lower Green River, or a combination of both. The lithology of all three reservoirs is similar; fractured sandstone, shale, limestone, and marlstone beds having generally low intergranular porosity and permeability. The strata were deposited in lacustrine and alluvial environments.
Bluebell Field Drill-hole Database, Duchesne and Uintah Counties, Utah
Author: Craig D. Morgan
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 34
Book Description
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 34
Book Description
Oil and Gas Production Maps of the Bluebell Field, Duchesne and Uintah Counties, Utah
Author: Craig D. Morgan
Publisher:
ISBN:
Category : Natural gas
Languages : en
Pages :
Book Description
Publisher:
ISBN:
Category : Natural gas
Languages : en
Pages :
Book Description
Second Annual Report, Increased Oil Production and Reserves from Improved Completion Techniques in the Bluebell Field, Uinta Basin, Utah
Author: Utah Geological and Mineral Survey
Publisher:
ISBN:
Category : Oil fields
Languages : en
Pages :
Book Description
Publisher:
ISBN:
Category : Oil fields
Languages : en
Pages :
Book Description
Upalco Unit/Uinta Basin Replacement Project, Duchesne County, Uintah County
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 624
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 624
Book Description
Increased Oil Production and Reserves from Improved Completion Techniques in the Bluebell Field, Uinta Basin, Utah
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages :
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages :
Book Description
Quarterly Review
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 76
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 76
Book Description
Uintah Unit Replacement Project, Central Utah Water Conservancy District, Duchesne County, Uintah County
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 602
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 602
Book Description
Quarterly Review - Utah Geological and Mineral Survey
Author: Utah Geological and Mineral Survey
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 62
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 62
Book Description
Shale oil resource play potential of the Green River Formation, Uinta Basin, Utah
Author: Steven Schamel
Publisher: Utah Geological Survey
ISBN:
Category : Energy minerals
Languages : en
Pages : 69
Book Description
The Green River Formation in the Uinta Basin has may characteristics typical of an ideal shale oil resource play. It is a world-class oil-prone source rock. In nearly all parts of the basin there are many thousands of net feet of Type-l and Type-ll kerogen-rich calcareous mudstones, many intervals of which have average total organic carbon (TOC) of 5-10% or greater. In the north-central and western parts of the basin a substantial part of the formation is in the oil-generative window. Furthermore, organic maturation simulations done in this study using PRA BasinView-3Dâ„¢ indicates early entry into the oil-generative window. In the northwest parts of the basin the lower Green River Formation was generating oil even before the end of the Eocene and slowing of sediment accumulation in the basin. The Green River Formation is unquestionably a superb petroleum system responsible for very large cumulative production of oil and associated natural gas, and an even larger potential oil sand resource. This DVD contains a 65-page report.
Publisher: Utah Geological Survey
ISBN:
Category : Energy minerals
Languages : en
Pages : 69
Book Description
The Green River Formation in the Uinta Basin has may characteristics typical of an ideal shale oil resource play. It is a world-class oil-prone source rock. In nearly all parts of the basin there are many thousands of net feet of Type-l and Type-ll kerogen-rich calcareous mudstones, many intervals of which have average total organic carbon (TOC) of 5-10% or greater. In the north-central and western parts of the basin a substantial part of the formation is in the oil-generative window. Furthermore, organic maturation simulations done in this study using PRA BasinView-3Dâ„¢ indicates early entry into the oil-generative window. In the northwest parts of the basin the lower Green River Formation was generating oil even before the end of the Eocene and slowing of sediment accumulation in the basin. The Green River Formation is unquestionably a superb petroleum system responsible for very large cumulative production of oil and associated natural gas, and an even larger potential oil sand resource. This DVD contains a 65-page report.