Zobrazeno 1 - 7
of 7
pro vyhledávání: '"C. O. Bowin"'
Publikováno v:
Solid Earth, Vol 6, Iss 3, Pp 1075-1085 (2015)
The new paradigm of plate tectonics began in 1960 with Harry H. Hess's 1960 realization that new ocean floor was being created today and is not everywhere of Precambrian age as previously thought. In the following decades an unprecedented coming toge
Externí odkaz:
https://doaj.org/article/b7c629d826d64169bd193be504d5c1f9
The global analysis of Bowin (2010) used the global 14 absolute Euler pole set (62 Myr history) from Gripp and Gordon (1990) and demonstrated that plate tectonics conserves angular momentum. We herein extend that analysis using the more detailed Bird
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad736db2de442286ca616b3bb7bc2d91
https://doi.org/10.5194/sed-7-1059-2015
https://doi.org/10.5194/sed-7-1059-2015
Publikováno v:
Journal of Geophysical Research: Solid Earth. 94:2883-2901
The broad topographic domes, or plateaus, of East Africa and Afar are characterized by long-wavelength negative Bouguer gravity anomalies and volcanically active rift valleys. Gravity and topography data from the East African and Afar plateaus and da
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::adea0a71263290066a320b2fbaeea8e7
https://doi.org/10.1029/jb094ib03p02883
https://doi.org/10.1029/jb094ib03p02883
Publikováno v:
Hot Brines and Recent Heavy Metal Deposits in the Red Sea ISBN: 9783662271209
Marine magnetic and gravity profile results over the hot brine area (21°30′N, 38°E) and axial trough of the Red Sea between 25°N and 18°N latitudes confirm previous hypotheses that dense, strongly magnetic rocks underlie these areas. The gravit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::87a2514605eef218bb34a594535f4e87
https://doi.org/10.1007/978-3-662-28603-6_10
https://doi.org/10.1007/978-3-662-28603-6_10
Publikováno v:
Geological Society of America Bulletin. 77:257
Three dredge hauls from the north wall of the Puerto Rico Trench near 66° 30′ W. contained serpentinized peridotite and talc rock, sedimentary rocks of Cretaceous and Tertiary age, and minor basalt. A possible stratigraphy of the main scarp is giv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f242f18c24cdf1c4b09e82d4c960c5a
https://doi.org/10.1130/0016-7606(1966)77[257:spftnw]2.0.co
https://doi.org/10.1130/0016-7606(1966)77[257:spftnw]2.0.co
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