By Warren I. Finch, A. C. Huffman Jr., James E. Fassett
About The Product
Published through the yankee Geophysical Union as a part of the Field journey Guidebooks Series.
The San Juan Basin of northwest New Mexico and south-west Colorado comprises large assets of subbituminous to bituminous coal, approximately half the U.S. uranium assets, the second one greatest natural-gas box within the conterminous usa, and several other huge oil fields. The uranium is focused in continental rocks of the higher Jurassic Morrison Formation in fundamental tabular and redistributed roll-type ore deposits. The coal and many of the oil and gasoline assets happen in transgressive-regressive rocks deposited in past due Cretaceous time at the southwestern fringe of the Western inside Seaway, mostly within the Dakota Sandstone, Mancos Shale, Mesaverde crew, Pictured Cliffs Sandstone, and Fruitland Formation. The journey will learn intimately some of the facies of the energy-producing Mesozoic rocks, that are good uncovered during this arid and lovely a part of the Colorado Plateau. excursions of mines will contain the Navajo coal strip mine west of Farmington, New Mexico, one of many greatest coal mines within the united states; the Lee Ranch coal strip mine, north of San Mateo, generating subbituminous coal from the Menefee Formation; and the Mt. Taylor underground uranium mine north of provides, New Mexico, generating ore from the most important fundamental ore deposit within the sector.
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Concerning the ProductPublished by way of the yankee Geophysical Union as a part of the sector journey Guidebooks sequence. The San Juan Basin of northwest New Mexico and south-west Colorado comprises large assets of subbituminous to bituminous coal, approximately 1/2 the U. S. uranium assets, the second one greatest natural-gas box within the conterminous usa, and a number of other huge oil fields.
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Additional resources for Coal, Uranium, and Oil and Gas in Mesozoic Rocks of the San Juan Basin: Anatomy of a Giant Energy-Rich Basin: Sandia Mountains to Mesita, New Mexico June 30-July 7, 1989
Source beds for Pennsylvanian oil and gas are believed to northern part of the basin reached maturity in the Eocene. Bond (1984) credited the Oligocene "heat flash" with eliminating the be organic-rich shales and laterally equivalent carbonates time consideration from maturation calculations for the Creta- within the Paradox. The presence of hydrogen sulfide (H,S) ceous section in the northern part of the basin where most of the and appreciable amounts of CO, at Barker Creek, Alkali Gulch, and Ute dome fields (fig.
Logo colorado lo*' 107' SURFACE WATER The San Juan Basin straddles the continental divide (fig. 1).
Its composition correlates with that of bitumen from the marine Mancos Shale. API gravity of Mesaverde oil ranges from 37" to 50". Pictured Cliffs Sandstone Hydrocarbon production from the regressive marine Upper Cretaceous Pictured Cliffs Sandstone has been primarily gas from stratigraphic traps in sandstone beds enclosed in shale or coal at the top of the unit. Stillstands or brief reversals in the regression of the Cretaceous sea to the northeast produced thicker shoreline sandstones, which have been the most productive.