Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Arturo Martín‐Barajas"'
Publikováno v:
Geofísica Internacional, Vol 44, Iss 1, Pp 103-111 (2005)
Laguna Salada in northern Baja California, Mexico, is an active half-graben product of the trans-tensional tectonics of the Gulf of California. It is sensitive to changes in sediment supply from the Colorado River basin. We present a time series anal
Externí odkaz:
https://doaj.org/article/927a9680ac7a43369a338bde9b88cba6
Pleistocene volcanism along the margins of the Canal de Ballenas transform fault, Gulf of California
Publikováno v:
Revista Mexicana de Ciencias Geológicas. 39:16-26
Pleistocene subaerial volcanism along the margins of the Ballenas Channel, northern Gulf of California, is represented by two morphologically young dacite dome complexes exposed at the opposite edges of sheared continental crust: Isla Coronado in coa
Autor:
Karina Fuentes, Juan Contreras, Florian Neumann, Raquel Negrete Aranda, Ronald M. Spelz, Ismael Yarbuh, Arturo Martín-Barajas, Mario González-Escobar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa1567cd9e97ab65ef1b380f86fc6eb1
https://doi.org/10.2139/ssrn.4454335
https://doi.org/10.2139/ssrn.4454335
Autor:
Justin T. Higa, Nathan D. Brown, Seulgi Moon, Joann M. Stock, Leah Sabbeth, Scott E. K. Bennett, Arturo Martín‐Barajas, Marina O. Argueta
Faults on microcontinents record the dynamic evolution of plate boundaries. However, most microcontinents are submarine and difficult to study. Here, we show that the southern part of the Isla Ángel de la Guarda (IAG) microcontinent, in the northern
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2e2dc41b78fe709b1d3c95d40060babd
https://resolver.caltech.edu/CaltechAUTHORS:20220203-136695400
https://resolver.caltech.edu/CaltechAUTHORS:20220203-136695400
Autor:
Adriana Miranda, A. L. Carreno, Arturo Martín-Barajas, Maritza Canache, Javier Helenes, Iraida Paredes, Juan Gabriel Flores-Trujillo
Publikováno v:
AAPG Bulletin. 103:1045-1069
The Vizcaino fore-arc basin accumulated approximately 4 km (∼13,000 ft) of upper Albian–middle Eocene siliciclastic marine sedimentary rocks derived from the Peninsular Ranges in Baja California. Data from eight exploratory wells document the mic
Publikováno v:
Revista Mexicana de Ciencias Geológicas. 39:206
In the above article, the data of the reference: Schmitt, A.K., Martín, A., Stockli, D., Farley, K.A., Lovera, O.M., 2013, (U-Th)/He zircon and archaeological ages for a late prehistoric eruption in the Salton Trough (California, USA): Geology, 2013
Autor:
Nathan D. Brown, Adriana Piña-Páez, Leah Sabbeth, Joann M. Stock, Arturo Martín-Barajas, Seulgi Moon
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Arturo Martín-Barajas, Alonso Sojo-Amezquita, Clemente G. Gallardo-Mata, Mario González-Escobar, Francisco Suárez-Vidal
Publikováno v:
International Geology Review. 56:1315-1331
The Gulf of California is an excellent example of how new ocean basins form. Tectonically, the northern Gulf of California is an incipient ocean basin and studies on it have defined acoustic basement and reveal the presence of new oceanic crust and i
Autor:
Arturo Martín-Barajas, John M. Fletcher, Michael E. Oskin, Rebecca J. Dorsey, Mario González-Escobar, Martín Pacheco
Publikováno v:
Tectonics. 32:1294-1311
[1] The transition from distributed continental extension to the rupture of continental lithosphere is imaged in the northern Gulf of California across the obliquely conjugate Tiburon-Upper Delfin basin segment. Structural mapping on a 5–20 km grid
Publikováno v:
International Geology Review. 54:1271-1283
Tiburon Basin is characterized by a thick sedimentary fill that records the evolution of one of the rift segments of the East Pacific Rise. Its structure corresponds to an echelon pull-apart basin bounded by two dextral-oblique faults. Unlike basins