Zobrazeno 1 - 10
of 21
pro vyhledávání: '"N. Onderdonk"'
Publikováno v:
Geosphere. 18:1804-1830
The western Transverse Ranges are a tectonically active mountain belt in southern California (USA) characterized by fast rates of shortening and rock uplift. Large drainages at the western end of this mountain belt, including the Santa Ynez River and
Autor:
N. Onderdonk
Contains PDF and radial plots of luminescence data (Item A), log-log plots of cumulative incision vs age for fluvial terraces (Item B), and profiles of terrace surfaces displaced by faults (Item C)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6e4c26a1ce871d40572a199a2067ec46
https://doi.org/10.1130/geos.s.21127603.v2
https://doi.org/10.1130/geos.s.21127603.v2
Autor:
Ian McGregor, N. Onderdonk
Publikováno v:
Geosphere. 17:932-956
The western Transverse Ranges and southern Coast Ranges of California are lithologically similar but have very different styles and rates of Quaternary deformation. The western Transverse Ranges are deformed by west-trending folds and reverse faults
Akademický článek
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Publikováno v:
Geosphere.
Publikováno v:
Lithosphere. 7:211-234
Most of the displacement across the North American−Pacific plate boundary in southern California is accommodated by the San Jacinto and the southern San Andreas fault zones. If and how the rate of displacement across these fault zones varies along
Publikováno v:
Bulletin of the Seismological Society of America. 103:2047-2061
We investigate a releasing stepover between the Casa Loma and Claremont strands of the northern San Jacinto fault zone to evaluate the late Quaternary structural evolution of the fault zone, and to assess the likelihood of a rupture jumping across th
Publikováno v:
Bulletin of the Seismological Society of America. 103:519-541
We present new data from the Mystic Lake paleoseismic site along the Claremont segment of the northern San Jacinto fault zone. The site is located within a sag formed between two fault strands that pass through the eastern side of Mystic Lake in the
Publikováno v:
Journal of Volcanology and Geothermal Research. 205:67-83
article i nfo The Salton Sea Geothermal System (California) is an easily accessible setting for investigating the interactions of biotic and abiogenic geochemical processes in sediment-hosted hydrothermal systems. We present new temperature data and
Publikováno v:
Geomorphology. 130:327-342
In the Salton Sea Geothermal Field in southern California, expulsion of gas, sediment and water creates unique geomorphic features similar to those seen on the surface of dormant mud volcanoes. These include pools of water or highly fluid mud named