From abstract: In the Sawatch, Mosquito and Front Ranges of central Colorado and the Sangre de Cristo Mountains of south-central Colorado, Tournaisian beds of the Mississippian Leadville Limestone overlie rocks of Early Mississippian and Late Devonian age. In the Sangre de Cristo Mountains in north-central New Mexico, the oldest beds are the Tournaisian (zone 9) Espiritu Santo Formation. In west-central New Mexico, in the Magdalena, Lemitar, and Ladron Mountains, the Kelly Limestone of Tournaisian and Visean age rests unconformably on Proterozoic metamorphic and igneous rocks. This report examines the stratigraphy of this area
The Sacramento Mountains constitute a sharply asymmetrical cuesta at the eastern edge of the Basin a...
From abstract: This report describes Cambrian through Mississippian rocks in the Powder River Basin ...
Geologic mapping, with an emphasis on structure, was carried out in the region of the headwaters of ...
The Sangre de Cristo Mountains of Colorado and New Mexico are, geologically speaking, relatively unk...
The early Paleozoic of northwestern and west-central Colorado is represented by continental shelf an...
From abstract: This report is about the geology of pre-Pennsylvanian rocks in the Paradox basin and ...
This report includes about seven square miles of the central front of the Fra Cristobal Mountains. T...
Abstract: The Oquirrh Group of Pennsylvanian and Permian age in the southern East Tintic Mountains, ...
Master of Science (MS)GeologyUniversity of Michiganhttp://deepblue.lib.umich.edu/bitstream/2027.42/1...
The area included in this survey is that part of New Mexico between (and adjacent to) U. S. Highways...
The Sacramento Mountains constitute a sharply asymmetrical cuesta at the eastern edge of the Basin a...
Approximately 5000 ft (1525 m) of strata crop out in the D Cross Mountain quadrangle in west-central...
PREVIOUS WORK Herrick (1904, p. 311) named the Mississippian strata of the Magdalena Mountains the &...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
Master of Science (MS)GeologyUniversity of Michiganhttp://deepblue.lib.umich.edu/bitstream/2027.42/1...
The Sacramento Mountains constitute a sharply asymmetrical cuesta at the eastern edge of the Basin a...
From abstract: This report describes Cambrian through Mississippian rocks in the Powder River Basin ...
Geologic mapping, with an emphasis on structure, was carried out in the region of the headwaters of ...
The Sangre de Cristo Mountains of Colorado and New Mexico are, geologically speaking, relatively unk...
The early Paleozoic of northwestern and west-central Colorado is represented by continental shelf an...
From abstract: This report is about the geology of pre-Pennsylvanian rocks in the Paradox basin and ...
This report includes about seven square miles of the central front of the Fra Cristobal Mountains. T...
Abstract: The Oquirrh Group of Pennsylvanian and Permian age in the southern East Tintic Mountains, ...
Master of Science (MS)GeologyUniversity of Michiganhttp://deepblue.lib.umich.edu/bitstream/2027.42/1...
The area included in this survey is that part of New Mexico between (and adjacent to) U. S. Highways...
The Sacramento Mountains constitute a sharply asymmetrical cuesta at the eastern edge of the Basin a...
Approximately 5000 ft (1525 m) of strata crop out in the D Cross Mountain quadrangle in west-central...
PREVIOUS WORK Herrick (1904, p. 311) named the Mississippian strata of the Magdalena Mountains the &...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
Master of Science (MS)GeologyUniversity of Michiganhttp://deepblue.lib.umich.edu/bitstream/2027.42/1...
The Sacramento Mountains constitute a sharply asymmetrical cuesta at the eastern edge of the Basin a...
From abstract: This report describes Cambrian through Mississippian rocks in the Powder River Basin ...
Geologic mapping, with an emphasis on structure, was carried out in the region of the headwaters of ...