Titlebook: Geology of the Northwest African Continental Margin; Ulrich Rad,Karl Hinz,Eugen Seibold Conference proceedings 1982 Springer-Verlag Berlin

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書(shū)目名稱Geology of the Northwest African Continental Margin影響因子(影響力)

書(shū)目名稱Geology of the Northwest African Continental Margin影響因子(影響力)學(xué)科排名

書(shū)目名稱Geology of the Northwest African Continental Margin網(wǎng)絡(luò)公開(kāi)度

書(shū)目名稱Geology of the Northwest African Continental Margin網(wǎng)絡(luò)公開(kāi)度學(xué)科排名

書(shū)目名稱Geology of the Northwest African Continental Margin被引頻次

書(shū)目名稱Geology of the Northwest African Continental Margin被引頻次學(xué)科排名

書(shū)目名稱Geology of the Northwest African Continental Margin年度引用

書(shū)目名稱Geology of the Northwest African Continental Margin年度引用學(xué)科排名

書(shū)目名稱Geology of the Northwest African Continental Margin讀者反饋

書(shū)目名稱Geology of the Northwest African Continental Margin讀者反饋學(xué)科排名

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Magnetic Anomalies in the Magnetic Quiet Zone off Moroccobserved further offshore, and in part the present shelf edge. The most westward anomaly is assumed to mark the initial rift zone, whereas the other anomalies lie on crust of continental origin. They may reveal a pattern of crustal weakness in this area.

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只看該作者 · 發(fā)表于 2025-3-22 09:26:11

Lens Distortion and Calibration,bserved further offshore, and in part the present shelf edge. The most westward anomaly is assumed to mark the initial rift zone, whereas the other anomalies lie on crust of continental origin. They may reveal a pattern of crustal weakness in this area.

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只看該作者 · 發(fā)表于 2025-3-22 20:53:45

只看該作者 · 發(fā)表于 2025-3-22 21:47:32

The Continental Margin of Morocco: Seismic Sequences, Structural Elements and Geological Developmentegment in the south, northward to the Tafelney Plateau, the Essaouira segment, the Mazagan Plateau, and the Pre-Rif segment..The dominating structural unit of the Moroccan continental margin is a NNE-trending zone of salt diapirs. This zone starts southeast of Fuerteventura and continues to the nort

只看該作者 · 發(fā)表于 2025-3-23 04:48:34

Magnetic Anomalies in the Magnetic Quiet Zone off Moroccotlantic coast of Morocco since 1967. The observed elongated anomalies in the magnetic quiet zone parallel in part the Mesozoic M-anomalies which are observed further offshore, and in part the present shelf edge. The most westward anomaly is assumed to mark the initial rift zone, whereas the other an

只看該作者 · 發(fā)表于 2025-3-23 06:41:41

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