The following report, by Peter J. Wyllie, Department of Geochemistry and Mineralogy, Pennsylvania State University, is based on a paper presented by the author at the Second Western National Meeting of the American Geophysical Union, held at Stanford University, December 1962. A similar, more-detailed version of this paper has been published in the Journal of Geophysical Research, August 1, 1963. The version presented below includes an enlarged discussion of possible applications to the orogenic cycle; essentially the same version has also been issued as Pennsylvania State University Mineral Industries Contribution No. 62-91
Geophysical (URSEIS experiment) and geological data from the Southern Uralides of central Russia pro...
Geophysical (URSEIS experiment) and geological data from the Southern Uralides of central Russia pro...
The concept that the Mohorovicic Discontinuity (Moho) does not necessarily coincide with the base of...
The available experimental data and steady-state calculations make it difficult to explain the M dis...
The available experimental data and steady-state calculations make it difficult to explain the M dis...
The available experimental data and steady-state calculations make it difficult to explain the M dis...
The temperature and pressure regime at the Mohorovicic discontinuity is developed for four specific ...
The temperature and pressure regime at the Mohorovicic discontinuity is developed for four specific ...
The temperature and pressure regime at the Mohorovicic discontinuity is developed for four specific ...
The temperature and pressure regime at the Mohorovicic discontinuity is developed for four specific ...
The formation of orogenic belts, like the Western Alps and the Himalayas, is an impressive manifesta...
Abstract: Regional metamorphism occurs in plate boundary zones. Accretionary orogenic systems form a...
The geological toolbox for the analysis of orogenic processes has seen substantial additions over th...
An overview of the modern progresses of the expanding Earth conceptions as they come out from new da...
This item is only available electronically.The intracratonic orogenesis of the Petermann Orogeny cau...
Geophysical (URSEIS experiment) and geological data from the Southern Uralides of central Russia pro...
Geophysical (URSEIS experiment) and geological data from the Southern Uralides of central Russia pro...
The concept that the Mohorovicic Discontinuity (Moho) does not necessarily coincide with the base of...
The available experimental data and steady-state calculations make it difficult to explain the M dis...
The available experimental data and steady-state calculations make it difficult to explain the M dis...
The available experimental data and steady-state calculations make it difficult to explain the M dis...
The temperature and pressure regime at the Mohorovicic discontinuity is developed for four specific ...
The temperature and pressure regime at the Mohorovicic discontinuity is developed for four specific ...
The temperature and pressure regime at the Mohorovicic discontinuity is developed for four specific ...
The temperature and pressure regime at the Mohorovicic discontinuity is developed for four specific ...
The formation of orogenic belts, like the Western Alps and the Himalayas, is an impressive manifesta...
Abstract: Regional metamorphism occurs in plate boundary zones. Accretionary orogenic systems form a...
The geological toolbox for the analysis of orogenic processes has seen substantial additions over th...
An overview of the modern progresses of the expanding Earth conceptions as they come out from new da...
This item is only available electronically.The intracratonic orogenesis of the Petermann Orogeny cau...
Geophysical (URSEIS experiment) and geological data from the Southern Uralides of central Russia pro...
Geophysical (URSEIS experiment) and geological data from the Southern Uralides of central Russia pro...
The concept that the Mohorovicic Discontinuity (Moho) does not necessarily coincide with the base of...