用户名  找回密码
 To register

QQ登录

只需一步,快速开始

扫一扫,访问微社区

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

[复制链接]
楼主: Madison
发表于 2025-3-25 04:28:20 | 显示全部楼层
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
发表于 2025-3-25 08:25:46 | 显示全部楼层
发表于 2025-3-25 13:32:03 | 显示全部楼层
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
发表于 2025-3-25 17:06:56 | 显示全部楼层
发表于 2025-3-25 21:40:57 | 显示全部楼层
,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
发表于 2025-3-26 01:04:11 | 显示全部楼层
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
发表于 2025-3-26 05:01:24 | 显示全部楼层
发表于 2025-3-26 10:53:18 | 显示全部楼层
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.
发表于 2025-3-26 16:39:08 | 显示全部楼层
发表于 2025-3-26 19:28:19 | 显示全部楼层
 关于派博传思  派博传思旗下网站  友情链接
派博传思介绍 公司地理位置 论文服务流程 影响因子官网 吾爱论文网 大讲堂 北京大学 Oxford Uni. Harvard Uni.
发展历史沿革 期刊点评 投稿经验总结 SCIENCEGARD IMPACTFACTOR 派博系数 清华大学 Yale Uni. Stanford Uni.
QQ|Archiver|手机版|小黑屋| 派博传思国际 ( 京公网安备110108008328) GMT+8, 2025-8-7 10:14
Copyright © 2001-2015 派博传思   京公网安备110108008328 版权所有 All rights reserved
快速回复 返回顶部 返回列表