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標(biāo)題: Titlebook: Geological Structures and Moving Plates; R. G. Park Book 1988 Springer Science+Business Media Dordrecht 1988 orogenic belt.orogeny.structu [打印本頁]

作者: 相持不下    時間: 2025-3-21 19:48
書目名稱Geological Structures and Moving Plates影響因子(影響力)




書目名稱Geological Structures and Moving Plates影響因子(影響力)學(xué)科排名




書目名稱Geological Structures and Moving Plates網(wǎng)絡(luò)公開度




書目名稱Geological Structures and Moving Plates網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Geological Structures and Moving Plates被引頻次




書目名稱Geological Structures and Moving Plates被引頻次學(xué)科排名




書目名稱Geological Structures and Moving Plates年度引用




書目名稱Geological Structures and Moving Plates年度引用學(xué)科排名




書目名稱Geological Structures and Moving Plates讀者反饋




書目名稱Geological Structures and Moving Plates讀者反饋學(xué)科排名





作者: 鍍金    時間: 2025-3-22 00:02

作者: 遠地點    時間: 2025-3-22 01:38
https://doi.org/10.1007/978-3-642-52602-2ements involving precise levelling and other techniques have shown that most parts of the crust are undergoing slow uplift or depression. The frequency and distribution of intraplate earthquakes is also an indication of widespread tectonic activity, albeit to a notably lesser degree than at plate boundaries.
作者: 侵略    時間: 2025-3-22 07:19

作者: 平庸的人或物    時間: 2025-3-22 12:11

作者: 高腳酒杯    時間: 2025-3-22 14:08
The lithosphere: some important properties,eanic crust is only about 7 km thick and could not remain undistorted when subjected to the horizontal stresses associated with plate tectonic processes. Plates must be therefore be considerably thicker than the crust and include part of the upper mantle as well.
作者: 高腳酒杯    時間: 2025-3-22 20:26
Plate movement and plate boundaries, to plate boundaries, where crustal deformation is therefore concentrated. The determination, both qualitatively and quantitatively, of the relative motion between two adjoining plates at their common boundary is therefore essential in understanding the deformation that takes place there.
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作者: Amylase    時間: 2025-3-23 10:52
https://doi.org/10.1007/978-3-663-09760-0form of localized rift zones and extensional basins, and are also frequently associated with the upper plates of subduction zones, as backarc extensional provinces. Strike-slip regimes typically involve local extensional provinces.
作者: 情感    時間: 2025-3-23 16:09
Divergent (extensional) tectonic regimes,form of localized rift zones and extensional basins, and are also frequently associated with the upper plates of subduction zones, as backarc extensional provinces. Strike-slip regimes typically involve local extensional provinces.
作者: 分開如此和諧    時間: 2025-3-23 21:17
978-0-412-74260-6Springer Science+Business Media Dordrecht 1988
作者: Parabola    時間: 2025-3-23 22:28

作者: 愚笨    時間: 2025-3-24 04:31
https://doi.org/10.34156/978-3-791-05851-1s idea was abandoned many years ago when it was realized that oceanic rocks could not behave in a sufficiently ductile manner near the surface. When the plate tectonic model was being developed in the 1960s, it was realized that the moving plates included oceanic as well as continental crust. The oc
作者: congenial    時間: 2025-3-24 08:19
,Italien – eine mafiose Demokratie?,es. We have seen that the plates have considerable lateral strength and suffer little lateral distortion over time periods of tens or even hundreds of Ma, and that they can transmit horizontal stresses through long distances in a regular fashion. We observe that large relative movements are confined
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作者: Ordeal    時間: 2025-3-25 02:11
https://doi.org/10.1007/978-3-642-52602-2ever it has always been recognized that this was only true to a first approximation, and that all regions of the Earth’s surface experience tectonic effects to some degree. The most common type of intraplate (within-plate) tectonic activity is undoubtedly vertical movements. Accurate geodetic measur
作者: 騷擾    時間: 2025-3-25 04:26

作者: tattle    時間: 2025-3-25 07:31
https://doi.org/10.1007/978-3-662-61723-6in time, beyond the period when accurate continental reconstructions can be made from oceanic palaeomagnetic data. This difficulty is magnified in the Precambrian because of the inherent inaccuracies of continental palaeomagnetic reconstructions, and is compounded by other problems. The familiar str
作者: 節(jié)省    時間: 2025-3-25 11:44

作者: 有雜色    時間: 2025-3-25 18:55

作者: 使激動    時間: 2025-3-25 22:33

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作者: Senescent    時間: 2025-3-26 22:51
Plate movement and plate boundaries,es. We have seen that the plates have considerable lateral strength and suffer little lateral distortion over time periods of tens or even hundreds of Ma, and that they can transmit horizontal stresses through long distances in a regular fashion. We observe that large relative movements are confined
作者: Asseverate    時間: 2025-3-27 02:30

作者: motivate    時間: 2025-3-27 07:11
Convergent tectonic regimes,Dewey and Bird (1970) in their classic paper ‘Mountain belts and the new global tectonics’. They demonstrated that the process of subduction at a destructive plate boundary inevitably produces a characteristic association of rocks and structures that, in pre-plate tectonic terminology, would have be
作者: Ointment    時間: 2025-3-27 12:46

作者: ticlopidine    時間: 2025-3-27 14:25
Intraplate tectonic regimes,ever it has always been recognized that this was only true to a first approximation, and that all regions of the Earth’s surface experience tectonic effects to some degree. The most common type of intraplate (within-plate) tectonic activity is undoubtedly vertical movements. Accurate geodetic measur
作者: 愉快嗎    時間: 2025-3-27 20:16
Phanerozoic orogenic belts: some examples,xamples, linking geological structure with plate movements and plate behaviour. In this and in the following chapter, we shall apply these principles and methods in order to understand the structure of certain orogenic belts. Obviously, very few belts can be discussed here, and much of the essential
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作者: debunk    時間: 2025-3-28 15:37
Bernd Rotherty, which gave rise to the theory that, even if you could offer no practical assistance, the mere ability to feel for another’s pain was a valuable characteristic, that somehow set you above the common, unfeeling herd — and was, in itself, a source of intense delight.
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