Zobrazeno 1 - 10
of 146
pro vyhledávání: '"Robert S. Coe"'
Autor:
Avto Goguitchaichvili, José Antonio González, Christopher J. Pluhar, Luis Alva-Valdivia, José Rosas Elguera, Vicente Carlos Ruiz Martinez, Jesús Solé, Xixi Zhao, Robert S. Coe, Cecilia Caballero
Publikováno v:
Geofísica Internacional, Vol 50, Iss 2, Pp 227-254 (2011)
Presentamos un estudio paleomagnético, de magnetismo de rocas geocronológico y de paleointensidad conjunto, en rocas volcánicas Miocénicas del sector oeste de la Faja Volcánica Transmexicana (FVTM). En el cual se emplearon 58 sitios compuestos p
Externí odkaz:
https://doaj.org/article/d1ea30d8a56146e3b78a22f7ecffef7f
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 9, Iss 11, Pp n/a-n/a (2008)
The Steens Basalt, now considered part of the Columbia River Basalt Group (CRBG), contains the earliest eruptions of this magmatic episode. Lava flows of the Steens Basalt cover about 50,000 km2 of the Oregon Plateau in sections up to 1000 m thick. T
Externí odkaz:
https://doaj.org/article/a374425b02e74003901e413dd5529bc9
The Searles Lake Formation in Searles Valley, southeastern California, represents deposition of the paleo–Owens River into a Pleistocene and Holocene pluvial terminal lake. A prior 32–10 ka estimated age for the upper part of the Searles Lake For
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4daf975956f1971c1b9457775afaf473
https://doi.org/10.1130/2018.2536(06)
https://doi.org/10.1130/2018.2536(06)
Publikováno v:
Geophysical Research Letters. 46:4182-4191
Greater India comprises a part of the Indian plate that subducted under Asia to help form the Tibetan Plateau. Defining the size of the Greater India is thus a key constraint to model the India-Asia collision, growth of the plateau, and the tectonic
Super-eruptions are amongst the most extreme events to affect Earth’s surface, but too few examples are known to assess their global role in crustal processes and environmental impact. We demonstrate a robust approach to recognize them at one of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e69c355fe24696f7b2f472f57348c883
Autor:
Peter U. Clark, Joseph S. Stoner, Robert S. Coe, Anthony A. P. Koppers, Andrea Balbas, K. Konrad, Brendan T Reilly
Publikováno v:
Geochemistry, Geophysics, Geosystems. 19:952-967
Changes in the Earth's magnetic field have global significance that reach from the outer core extending out to the uppermost atmosphere. Paleomagnetic records derived from sedimentary and volcanic sequences provide important insights into the geodyna
Publikováno v:
Physics of the Earth and Planetary Interiors. 318:106769
Anhysteretic remanent magnetization (ARM) data serve many applications in the geosciences, such as quantifying the paleomagnetic field intensity, the magnetic grain size distributions in rocks, the degree of particle alignment from flow processes, an
Autor:
Jun Meng, Xixi Zhao, Pengfei Ma, Yalin Li, Stuart Gilder, Robert S. Coe, Shuai Li, Hao Liu, Chengshan Wang, Kai Shi
Publikováno v:
Geophysical Research Letters. 44:6624-6632
Understanding the dynamics of double-thickening and uplifting of the Tibetan crust requires constraints on the magnitude and timing of crustal shortening. New elongation/inclination (E/I)-corrected paleomagnetic data from similar to 26-22 Ma sediment
Synchronizing volcanic, sedimentary, and ice core records of Earth’s last magnetic polarity reversal
Publikováno v:
Science Advances
Earth’s last magnetic field reversal was complex, with excursions at 795 and 784 ka before a final polarity flip at 773 ka.
Reversal of Earth’s magnetic field polarity every 105 to 106 years is among the most far-reaching, yet enigmatic, geo
Reversal of Earth’s magnetic field polarity every 105 to 106 years is among the most far-reaching, yet enigmatic, geo
Publikováno v:
Comptes Rendus Geoscience. 348:551-560
Measuring the intensity of the Moon's ancient magnetic field is an important goal of lunar sample analysis. Paleointensity estimates using thermal methods (Thellier–Thellier) raise the problem of sample alteration, especially for lunar samples carr