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Titlebook: Oceanic Hotspots; Intraplate Submarine Roger Hekinian,Jean-Louis Cheminée,Peter Stoffers Book 2004 Springer-Verlag Berlin Heidelberg 2004 I

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樓主: Adams
31#
發(fā)表于 2025-3-26 21:35:09 | 只看該作者
Ridge Suction Drives Plume-Ridge Interactions,egantly illustrate this concept. For example, the origin of oceanic plates at ocean ridges, the movement and growth of these plates, and their ultimate consumption back into the Earth’s interior through subduction zones provide an efficient mechanism to cool the Earth’s mantle, leading to large-scal
32#
發(fā)表于 2025-3-27 02:45:33 | 只看該作者
Intraplate Gabbroic Rock Debris Ejected from the Magma Chamber of the Macdonald Seamount (Austral Hosely monitored by the detection of seismic swarms recorded by the French Polynesian seismic network (“Réseau Sismique Polynésien”, .). Since the Austral Islands are too far away from the receiving stations, only ‘T’ waves have been detected from the Macdonald Seamount (.; see Sects. 2.4.1 and 2.4.2
33#
發(fā)表于 2025-3-27 07:45:47 | 只看該作者
The Foundation Chain: Inferring Hotspot-Plate Interaction from a Weak Seamount Trail,s a ~1350 km long chain of seamounts trending approximately in the direction of the absolute motion of the Pacific Plate (.)Fig. 11.1. A significant section of the Foundation Chain lies in a tectonic setting influenced by a change in the direction of sea-floor spreading between 26 and 11 Ma (.; .; .
34#
發(fā)表于 2025-3-27 12:41:05 | 只看該作者
Hydrothermal Iron and Manganese Crusts from the Pitcairn Hotspot Region,types (.; .): (1) hydrogenetic, (2) diagenetic, and (3) hydrothermal. Hydrogenetic deposits occur as crusts on seamounts and other volcanic outcrops and as nodules on abyssal sediments via the direct precipitation of ironmanganese oxides and hydroxides from seawater (.). Since these oxides and hydro
35#
發(fā)表于 2025-3-27 13:38:50 | 只看該作者
36#
發(fā)表于 2025-3-27 18:03:25 | 只看該作者
Petrology of Young Submarine Hotspot Lava: Composition and Classification,ainly extrudes basaltic rocks. The mineralogical and chemical compositions of oceanic rocks are important factors that affect the formation of the oceanic crust, because the rock’s composition influences its rate of extrusion, the morphology of lava flows, the cooling rate, the mode of emplacement,
37#
發(fā)表于 2025-3-27 22:14:58 | 只看該作者
38#
發(fā)表于 2025-3-28 04:02:05 | 只看該作者
39#
發(fā)表于 2025-3-28 08:09:55 | 只看該作者
40#
發(fā)表于 2025-3-28 12:25:04 | 只看該作者
V. Clouard,A. Bonnevilleerte mathematische Formeln, Grafiken oder Tabellen.Das Buch .Im betrieblichen Alltag z?hlen vor allem die gro?en wirtschaftlichen Zusammenh?nge. Doch diese gehen im BWL-Studium meist in einer wahren Detailflut verloren. In der Praxis sind zudem gerade die einfachen Dinge entscheidend, die w?hrend de
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