Add to ORKGThis paper is a brief resume of the Escabrosa Group and Paradise Formation of extreme southwestern New Mexico. For detailed information on the Mississippia
Recognition of the Mississippian sequence exposed at North Georgetown Canyon, Idaho, as a facies bel...
The Sacramento Mountains constitute a sharply asymmetrical cuesta at the eastern edge of the Basin a...
ABSTRACT—Twenty-three species of trilobites are recognized in the lower Mississippian Caballero and ...
PREVIOUS WORK Herrick (1904, p. 311) named the Mississippian strata of the Magdalena Mountains the &...
Vita.Mississippian (Kinderhookian-Chesterian) strata in the San Andres and Sacramento Mountains of s...
Where now the blistering summer sun sends waves of heat over the desert sands, once rolled cool salt...
Little detailed work has been published on the Mesozoic stratigraphy of south-central New Mexico, bu...
The Mississippian system confined to the subsurface between depths of 7,100 and 12,650 feet is compo...
From abstract: In the Sawatch, Mosquito and Front Ranges of central Colorado and the Sangre de Crist...
The Lower Permian (Wolfcampian) Hueco Formation in the Dona Ana Mountains of south-central New Mexic...
Formational units of the Meramec Series are present only in the southwestern portion and along the s...
The Late Mississippian (~330 Ma) was a period of global climate change. During this period southwest...
The detailed sequence stratigraphy of lower and middle Mississippian rocks in southwestern Missouri ...
The study of the pre-Mesozoic geological history of NE Mexico offers the opportunity to reconstruct ...
Relative sea level stand and sedimentation in the Late Pennsylvanian and Early Permian Pedregosa bas...
Recognition of the Mississippian sequence exposed at North Georgetown Canyon, Idaho, as a facies bel...
The Sacramento Mountains constitute a sharply asymmetrical cuesta at the eastern edge of the Basin a...
ABSTRACT—Twenty-three species of trilobites are recognized in the lower Mississippian Caballero and ...
PREVIOUS WORK Herrick (1904, p. 311) named the Mississippian strata of the Magdalena Mountains the &...
Vita.Mississippian (Kinderhookian-Chesterian) strata in the San Andres and Sacramento Mountains of s...
Where now the blistering summer sun sends waves of heat over the desert sands, once rolled cool salt...
Little detailed work has been published on the Mesozoic stratigraphy of south-central New Mexico, bu...
The Mississippian system confined to the subsurface between depths of 7,100 and 12,650 feet is compo...
From abstract: In the Sawatch, Mosquito and Front Ranges of central Colorado and the Sangre de Crist...
The Lower Permian (Wolfcampian) Hueco Formation in the Dona Ana Mountains of south-central New Mexic...
Formational units of the Meramec Series are present only in the southwestern portion and along the s...
The Late Mississippian (~330 Ma) was a period of global climate change. During this period southwest...
The detailed sequence stratigraphy of lower and middle Mississippian rocks in southwestern Missouri ...
The study of the pre-Mesozoic geological history of NE Mexico offers the opportunity to reconstruct ...
Relative sea level stand and sedimentation in the Late Pennsylvanian and Early Permian Pedregosa bas...
Recognition of the Mississippian sequence exposed at North Georgetown Canyon, Idaho, as a facies bel...
The Sacramento Mountains constitute a sharply asymmetrical cuesta at the eastern edge of the Basin a...
ABSTRACT—Twenty-three species of trilobites are recognized in the lower Mississippian Caballero and ...