Add to ORKGFrom abstract: Siliciclastic and minor carbonate rocks of the lower part of the Middle Pennsylvanian Minturn Formation of north-central Colorado were deposited in alluvial-fan, braidplain, Gilbert-delta, shoreline, and paralic, and offshore-marine environments. These strata can be divided into twelve genetic sequences that are generally bounded by transgressive surfaces of erosion or paralic flooding surfaces, and are characterized by thin and thick transgressive units. This report examines the paleogeography of this area
In southeastern Kansas, the Middle Pennsylvanian (Desmoinesian) Bandera Shale consists of sandstone,...
Late Paleozoic and modern feldspathic clastic sediments of the Colorado Rockies were derived from do...
From abstract: In the Sawatch, Mosquito and Front Ranges of central Colorado and the Sangre de Crist...
Field study of the middle part of the Pennsylvanian Minturn Formation in the McCoy-Bond area of nort...
The early Paleozoic of northwestern and west-central Colorado is represented by continental shelf an...
Sedimentological and structural data from Pennsylvanian-Permian synorogenic deposits of the Central ...
The Fort Worth Basin, a marginal foreland basin of the Ouachita orogenic belt was a site of sediment...
The lower Rocky Mountain Supergroup of Pennsylvanian age contains five formations which in ascending...
The exposures of the Mesaverde Formation at Rifle Gap, Colorado, are of a regressive series of marin...
From abstract: This report describes Cambrian through Mississippian rocks in the Powder River Basin ...
From abstract: This report is about the geology of pre-Pennsylvanian rocks in the Paradox basin and ...
The strata on the Colorado Plateau preserve some of the most extensively, successively exposed and w...
The strata of Pennsylvanian age in north-central Texas dip gently and uniformly to the northwest. Th...
1990 Summer.Includes bibliographical references (pages [143]-151).Includes plates.Deposition of the ...
The Colorado River has flowed across the dextral strike-slip plate boundary between the North Americ...
In southeastern Kansas, the Middle Pennsylvanian (Desmoinesian) Bandera Shale consists of sandstone,...
Late Paleozoic and modern feldspathic clastic sediments of the Colorado Rockies were derived from do...
From abstract: In the Sawatch, Mosquito and Front Ranges of central Colorado and the Sangre de Crist...
Field study of the middle part of the Pennsylvanian Minturn Formation in the McCoy-Bond area of nort...
The early Paleozoic of northwestern and west-central Colorado is represented by continental shelf an...
Sedimentological and structural data from Pennsylvanian-Permian synorogenic deposits of the Central ...
The Fort Worth Basin, a marginal foreland basin of the Ouachita orogenic belt was a site of sediment...
The lower Rocky Mountain Supergroup of Pennsylvanian age contains five formations which in ascending...
The exposures of the Mesaverde Formation at Rifle Gap, Colorado, are of a regressive series of marin...
From abstract: This report describes Cambrian through Mississippian rocks in the Powder River Basin ...
From abstract: This report is about the geology of pre-Pennsylvanian rocks in the Paradox basin and ...
The strata on the Colorado Plateau preserve some of the most extensively, successively exposed and w...
The strata of Pennsylvanian age in north-central Texas dip gently and uniformly to the northwest. Th...
1990 Summer.Includes bibliographical references (pages [143]-151).Includes plates.Deposition of the ...
The Colorado River has flowed across the dextral strike-slip plate boundary between the North Americ...
In southeastern Kansas, the Middle Pennsylvanian (Desmoinesian) Bandera Shale consists of sandstone,...
Late Paleozoic and modern feldspathic clastic sediments of the Colorado Rockies were derived from do...
From abstract: In the Sawatch, Mosquito and Front Ranges of central Colorado and the Sangre de Crist...