The ocean basins : their structure and evolution prepared by John Wright and David A. Rothery (Oceanography series, v. 1) Butterworth-Heinemann, in associetion with the Open University ,1998 2nd ed. / revised for the course team by David A. Rothery...
Geological mapping and gravity surveying were used to constrain the shape of the Serravallian and Tortonian (U. Miocene) rocks of the Sorbas basin, SE Spain, and hence its tectonic evolution and place in the overall regional tectonic scheme. The present-day basin floor forms a westerly-deepeni...
Earth's surface evolution is characterized by tectonic motions of rigid plates. The majority of continental lithosphere can aggregate into one body to form a supercontinent. The generally accepted supercontinents include Nuna (ca. 1600–1400 Ma), Rodinia (ca. 900–700 Ma), Pangea (ca. 320–200...
Tectonic history of the Bering Sea and evolution of strike-slip basins of the Bering Shelf Bowers ridge is a totally submerged projection of the central Aleutian Islands ridge that extends counterclockwise into the Bering Sea, separating Bowers b... Worrall,M Dan - 《Geological Society of America...
P., 1971, Evolution of the Central Indian Ridge, Western Indian Ocean, Geol. Soc. Amer. Bull. 82, 553–562. Lowrie, W. and Alvarez, W., 1981, One Hundred Million Years of Geomagnetic Polarity History, Geology 9, 392–397. Macdonald, K. C., 1982, Mid-Ocean Ridges: Fine Scale ...
Rexer-Huber K, Veale AJ, Catry P, Cherel Y, Dutoit L, Foster Y, McEwan JC, Parker GC, Phillips RA, Ryan PG, Stanworth AJ, van Stijn T, Thompson DR, Water J, Robertson BC (2019) Genomics detects population structure within and between ocean basins in a circumpolar seabird: the white...
The breakup of Pangea in the Jurassic saw the opening of major ocean basins at the expense of older Tethyan and Pacific oceanic plates. Although the Tethyan seafloor spreading history has been lost to subduction, proxy indicators from multiple generations of Tethyan ribbon terranes and the active ...
How much do we understand the structure and evolution of the Salton Trough? The Salton Trough, at the northern end of the Gulf of California, likely formed by different processes than the central and southern Gulf due to the weak rheology of its thick quartz-rich sedimentary fill and its ...
The structure and evolution of deepwater basins in the distal margin of the northern South China Sea and their implications for the formation of the continental margin 热度: The Sexual Key - How To Use The Structure Of Female Emotion To Arouse A Woman In Minutes 热度: An Analysis of ...
Crustal structure derived primarily from geophysical investigations reveals features that may be related to the complex tectonic evolution of the Tornquist Fan region. This northwestwards widening splay of Late Carboniferous - Early Permian fault zones in the Danish region emanates from the Teisseyre-...