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Hui Yang, Jinhong Liu, Leichao Bai and Mingliang Luo
The development of loess landforms is controlled by underlying, pre-existing paleotopography. Previous studies have focused on the inheritance of loess landform and the control of underlying paleotopography on modern terrain based on the digital elevatio...
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Lance D. Yarbrough, Rian A. Engle and Greg Easson
The Upper Jurassic (Oxfordian Age) Smackover Formation is a significant source for hydrocarbon production in southwest Alabama. Brooklyn Field is in southeast Conecuh County, Alabama, and has been a major producer of oil and natural gas for the state. Th...
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Jorge Quezada,Jose Luis Cerda,Arturo Jensen
Pág. 78 - 109
This work analyzes the morphological features of the western margin of the northern Chile Coastal Cordillera, characterized by the presence of a major Coastal Cliff. The main purpose of this research is to better understand the tectonic and climatic cont...
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Jesus A. Sanchez,Jacobus P. Le Roux
Pág. 143 - 157
The Magellan Block, located on the modern Atlantic continental platform opposite the Strait of Magellan (Chile), consists of two parallel, northwest trending horsts partly separated by a central graben. Petroleum has been recovered from the Springhill Fo...
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Wes Hildreth,Judy Fierstein,Estanislao Godoy,Robert E. Drake,Brad Singer
Pág. 275 - 309
A remote volcanic field in the rugged headwaters of the Río Puelche and Río Invernada (35.8°S) constitutes the largest cluster of Quaternary rhyolite lava flows yet identified in the Andean Southern Volcanic Zone. The Puelche Volcanic Field belongs to an...
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Jean Francois Dumont,Jose Arana
Pág. 15 - 20
Resumen. El piedemonte de los Andes Orientales del Peru Central se caracteriza, en San Ramon, por la acumulacion de capas aluviales conglomeradicas (Formacion Canon) en una paleotopograffa diferenciada, probablemente, al comienzo del Plioceno (Cuenca de ...
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