標題: Titlebook: Oceanic Basalts; P. A. Floyd Book 1991 Blackie and Son Ltd 1991 environment.formation.gas.geology.igneous rock.mineral.mineralogy.petrogen [打印本頁] 作者: 清楚明確 時間: 2025-3-21 17:06
書目名稱Oceanic Basalts影響因子(影響力)
書目名稱Oceanic Basalts影響因子(影響力)學(xué)科排名
書目名稱Oceanic Basalts網(wǎng)絡(luò)公開度
書目名稱Oceanic Basalts網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Oceanic Basalts被引頻次
書目名稱Oceanic Basalts被引頻次學(xué)科排名
書目名稱Oceanic Basalts年度引用
書目名稱Oceanic Basalts年度引用學(xué)科排名
書目名稱Oceanic Basalts讀者反饋
書目名稱Oceanic Basalts讀者反饋學(xué)科排名
作者: 捐助 時間: 2025-3-21 23:58 作者: gratify 時間: 2025-3-22 04:00 作者: Flounder 時間: 2025-3-22 04:40 作者: TSH582 時間: 2025-3-22 11:08
978-94-010-5353-2Blackie and Son Ltd 1991作者: BLOT 時間: 2025-3-22 15:26 作者: 發(fā)起 時間: 2025-3-22 20:10 作者: 征兵 時間: 2025-3-22 22:53
Oceanic islands and seamountshot-spot aetivity are sited on large-scale topographic swells (1000–2000 km in width) that elevate some volcanic domains 1–2 km above the adjacent seafloor (Monnereau and Cazenave, 1988; White, 1989). The geophysical properties of swells (e.g. geoid, gravity and heat flow anomalies) suggest that the作者: 壯麗的去 時間: 2025-3-23 05:25 作者: Axon895 時間: 2025-3-23 08:58
ater via hydrothermal activity. Compositional variations displayed by oceanic basalts provide windows into the mantle, and the identification of isotopically-distinct mantle reservoirs demonstrates that the source of oceanic basalts is heterogeneous and is controlled by convection and reservoir interactions w978-94-010-5353-2978-94-011-3042-4作者: adequate-intake 時間: 2025-3-23 12:37
Introduction and the ophiolite modelnd the Mediterranean islands. When Darwin landed on St Paul’s Rocks in the equatorial Atlantic from the . in 1831, he could recognize the anomaly of the peridotite mylonites that he found there. These mylonites are the only subaerial outcrop of an active oceanic transform fault zone, although that p作者: 臥虎藏龍 時間: 2025-3-23 16:35 作者: candle 時間: 2025-3-23 21:05 作者: 激勵 時間: 2025-3-24 01:23
Structure of the oceanic crust as deduced from ophiolitese and there are limitations to the depths penetrable by drilling (currently about 1 km below the seafloor). Our current knowledge of crustal structure is based on three sources of information: (1) rock samples obtained by submersibles and from oceanic islands, drill core and dredge hauls; (2) geophy作者: nutrients 時間: 2025-3-24 05:04
Mineralogy and crystallization of oceanic basaltsce on our planet, covering nearly two-thirds of the earth’s surface beneath the oceans. Three decades ago, the lavas of the oceanic ridges were virtually unknown and unsampled. Today, major portions of the ocean ridge system in the Atlantic, Pacific and Indian Oceans have been dredged, drilled and s作者: cogent 時間: 2025-3-24 10:00
Experimental phase petrology of mid-ocean ridge basaltsn equilibrium with basaltic liquids under a variety of magmatic conditions. These experimental studies generally fall into two major groups, those at low pressures (generally at 1 atm (1 atm = 101 325 N m .), but sometimes 2–3 kbar (1 bar= 10. N m .)) and those at high pressures (generally about 8–3作者: white-matter 時間: 2025-3-24 13:40
Magmatic processes in oceanic ridge and intraplate settingsThe oceanic lithosphere also contains islands and archipelagos representing the effects of isolated, but durable, mantle melting anomalies. In attempting to review the processes of magma genesis and evolution in these distinctive environments, this chapter draws on existing syntheses of magmatic pro作者: 在前面 時間: 2025-3-24 16:29
Metamorphic and hydrothermal processes: basalt—seawater interactions. Part II of this book discusses the importance of many of these initial basalt properties and how their measurement can be interpreted to infer the source, melting history, magmatic evolution and volcanic processes which formed the oceanic basalts. This chapter discusses how these properties can be作者: gospel 時間: 2025-3-24 20:41 作者: 全面 時間: 2025-3-25 03:02 作者: 熱情贊揚 時間: 2025-3-25 05:28
Pacific ocean crustrgest and fastest moving plate, the Pacific plate, in addition to the smaller Nazca, Cocos, Rivera, Juan de Fuca, Gorda and Explorer plates, three so-called micropiates (Galapagos, Easter and Juan Fernandez), plus portions of neighbouring plates in the south and south-west Pacific (Figure 11.1). Des作者: 值得尊敬 時間: 2025-3-25 10:33
Indian ocean crust detailed petrographic observations and mineral chemistry. The mineralogical aspects and the magmatic processes envisaged can be considered as adjunct topics to Chapters 5 and 7, respectively, in Part II. The first section considers the consequences of the existence of magmatic lineages, which are p作者: 腐爛 時間: 2025-3-25 14:25 作者: staging 時間: 2025-3-25 19:48
Oceanic peridotitest the island was not of volcanic origin. Around the turn of the century peridotites broadly similar to those on St. Paul’s rocks were found as basalt- and kimberlite-borne xenoliths in ocean basins and on continental crust. Indeed it was the correlation between the seismic properties of such ultrama作者: Instrumental 時間: 2025-3-25 20:23 作者: UTTER 時間: 2025-3-26 00:31
Introduction and the ophiolite modely to land-bound lay people the great depth of the oceans, the fundamental differences between continents and oceans, and the constant renewal of the ocean floor by seafloor spreading and subduction, when their concepts are bounded by a wrinkled sea surface viewed from the air. In the early nineteenth century such ideas lay beyond everyone’s grasp.作者: 捕鯨魚叉 時間: 2025-3-26 07:05 作者: slow-wave-sleep 時間: 2025-3-26 08:56
Metamorphic and hydrothermal processes: basalt—seawater interactions changed, and the resulting metamorphosis and evolution of the oceanic crust as it ages and passes from its place of origin at the accreting plate margin to its eventual return to the mantle at subduction zones.作者: 使服水土 時間: 2025-3-26 13:10
Back-arc basinssis in many tectonic settings. The study of magmatism at destructive plate boundaries provides important information about the scale of crustal recycling, which may in time influence our understanding of the evolution of the crust and mantle.作者: reception 時間: 2025-3-26 19:25 作者: 配置 時間: 2025-3-26 23:02
North Atlantic ocean crust and Icelandcerning the nature of the mantle under this ocean basin. Coverage of the South Atlantic Ocean is not within the scope of this chapter, but details can be found in Schilling . (1984), Le Roex . (1985a, b), Chaffey . (1989), Sun and McDonough (1989), ODP Leg 108 and references cited therein.作者: 雄辯 時間: 2025-3-27 03:40 作者: 細菌等 時間: 2025-3-27 06:03 作者: finale 時間: 2025-3-27 12:30 作者: pulse-pressure 時間: 2025-3-27 15:30
Structure of the oceanic crust as deduced from ophiolites is based on three sources of information: (1) rock samples obtained by submersibles and from oceanic islands, drill core and dredge hauls; (2) geophysical data; and (3) subaerially exposed fragments of ocean crust and upper mantle, that is, ophiolites (Chapter 1).作者: 重疊 時間: 2025-3-27 19:45 作者: 能夠支付 時間: 2025-3-28 00:59
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