Deposits of Tertiary age are extensively developed in New Mexico. The greatest thicknesses are found in the northwestern and central parts of the state, where their maximum measurements reach no less than 3,000 feet. Many minor areas are also known. These deposits recline usually in marked unconformity upon the beveled edges of the Cretaceous and older strata. They are geologically among the most important deposits of the region
The border region between Coahuila and Zacatecas is part of the mountainous country south of Parras ...
A well-constrained age model is a critical piece of information in geologic studies. This dissertati...
textThe geologic map of El Cuervo area shows distribution of stratigraphic units ranging in age from...
Deposits of Tertiary age are extensively developed in New Mexico. The greatest thicknesses are found...
Approximately 5000 ft (1525 m) of strata crop out in the D Cross Mountain quadrangle in west-central...
p. 57-67, [3] leaves of plates (1 folded) : ill., map ; 24 cm.Includes bibliographical references.Ne...
Cenozoic sedimentary rocks could be designated as those rocks everywhere underfoot, but rarely seen ...
Reconnaissance field work has led to the recognition of extensive Early Tertiary gneiss and schist w...
p. 617-635, [7] leaves of plates (1 folded) : ill., maps ; 24 cm.Includes bibliographical references...
The Dakota Group surrounding Las Vegas, New Mexico, consists of three units: 1) a basal, predominate...
For a long time after the vast coal fields which extend around the southern extremity of the Rocky M...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
The Lone Star deposit is located in La Bajada Canyon in western Santa Fe County, New Mexico. The exp...
textThe stratigraphic relationship of Lower Cretaceous rocks in northern Mexico is poorly understood...
The Late Cretaceous-Paleogene Mexican foreland basin (MFB), defined herein, represents the southern ...
The border region between Coahuila and Zacatecas is part of the mountainous country south of Parras ...
A well-constrained age model is a critical piece of information in geologic studies. This dissertati...
textThe geologic map of El Cuervo area shows distribution of stratigraphic units ranging in age from...
Deposits of Tertiary age are extensively developed in New Mexico. The greatest thicknesses are found...
Approximately 5000 ft (1525 m) of strata crop out in the D Cross Mountain quadrangle in west-central...
p. 57-67, [3] leaves of plates (1 folded) : ill., map ; 24 cm.Includes bibliographical references.Ne...
Cenozoic sedimentary rocks could be designated as those rocks everywhere underfoot, but rarely seen ...
Reconnaissance field work has led to the recognition of extensive Early Tertiary gneiss and schist w...
p. 617-635, [7] leaves of plates (1 folded) : ill., maps ; 24 cm.Includes bibliographical references...
The Dakota Group surrounding Las Vegas, New Mexico, consists of three units: 1) a basal, predominate...
For a long time after the vast coal fields which extend around the southern extremity of the Rocky M...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
The Lone Star deposit is located in La Bajada Canyon in western Santa Fe County, New Mexico. The exp...
textThe stratigraphic relationship of Lower Cretaceous rocks in northern Mexico is poorly understood...
The Late Cretaceous-Paleogene Mexican foreland basin (MFB), defined herein, represents the southern ...
The border region between Coahuila and Zacatecas is part of the mountainous country south of Parras ...
A well-constrained age model is a critical piece of information in geologic studies. This dissertati...
textThe geologic map of El Cuervo area shows distribution of stratigraphic units ranging in age from...