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Titlebook: Rifted Ocean-Continent Boundaries; E. Banda,M. Torné,M. Talwani Book 1995 Springer Science+Business Media Dordrecht 1995 Atlantic Ocean.Co

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樓主: Madison
21#
發(fā)表于 2025-3-25 04:28:20 | 只看該作者
Lithospheric Transition from Continental to Oceanic in the West Iberia Atlantic Margin,dicular to the margin from the deep ocean to the continental platform. The profiles cut across the Iberian and Tagus Abyssal Plains, respectively. The lithospheric modelling, which is based on finite element technique, combines elevation, heat flow, and gravity data. This together with the computati
22#
發(fā)表于 2025-3-25 08:25:46 | 只看該作者
23#
發(fā)表于 2025-3-25 13:32:03 | 只看該作者
Mapping the Moho in the Iberian Mediterranean Margin by Multicoverage Processing and Merging of Widiments include in-line recordings onshore of marine profiles, and provide coincident small and large-offset multicoverage of complex areas such as the onshore/offshore transition, where classic stacked images of the vertical reflectivity lack resolution and hamper a thorough comprehension of the str
24#
發(fā)表于 2025-3-25 17:06:56 | 只看該作者
25#
發(fā)表于 2025-3-25 21:40:57 | 只看該作者
,The Cote D’Ivoire — Ghana Transform Margin: An Example of an Ocean-Continent Transform Boundary,late boundaries and are less understood than the two other major plate boundaries, (divergent and convergent). Secondly, the precise study of transfonn margins can help in better constraining the structure and evolution of the ocean-continent transfonn boundary, particularly the history of the defon
26#
發(fā)表于 2025-3-26 01:04:11 | 只看該作者
Backarc Evolution and Ophiolite Formation, to discuss a possible relationship between the opening of the Japan Sea and the formation of the Ophiolite belt. It is speculated that the Ophiolite belt was formed by slicing of the lithosphere and uplift of serpentinized mantle peridotite in Miocene times. Slicing of the lithosphere was induced b
27#
發(fā)表于 2025-3-26 05:01:24 | 只看該作者
28#
發(fā)表于 2025-3-26 10:53:18 | 只看該作者
Backarc Evolution and Ophiolite Formation,belt was formed by slicing of the lithosphere and uplift of serpentinized mantle peridotite in Miocene times. Slicing of the lithosphere was induced by the opening of the Shikoku Basin (a part of the Philippine Sea Plate) shortly after the opening of the Japan Sea.
29#
發(fā)表于 2025-3-26 16:39:08 | 只看該作者
30#
發(fā)表于 2025-3-26 19:28:19 | 只看該作者
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