Titlebook: JIMD Reports - Volume 10; Johannes Zschocke,K Michael Gibson,Verena Peters Book 2013 SSIEM and Springer-Verlag Berlin Heidelberg 2013 endo

Cleveland

書目名稱JIMD Reports - Volume 10影響因子(影響力)




書目名稱JIMD Reports - Volume 10影響因子(影響力)學科排名




書目名稱JIMD Reports - Volume 10網(wǎng)絡公開度




書目名稱JIMD Reports - Volume 10網(wǎng)絡公開度學科排名




書目名稱JIMD Reports - Volume 10被引頻次




書目名稱JIMD Reports - Volume 10被引頻次學科排名




書目名稱JIMD Reports - Volume 10年度引用




書目名稱JIMD Reports - Volume 10年度引用學科排名




書目名稱JIMD Reports - Volume 10讀者反饋




書目名稱JIMD Reports - Volume 10讀者反饋學科排名

Ligament

開玩笑

一再煩擾

Adela Della Marina,Ulrike Schara,Angela Pyle,Claudia M?ller-Hartmann,Elke Holinski-Feder,Angela Abice have even less reason to be satisfied with the Lin-Shu-Kalnajs analysis of (140) which, unaided, is unable to give an adequate account of even the high-frequency normal modes; Personne‘s programme turns out to involve loosely-wound waves for which the LsK-dispersion relation is not really valid. O

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Teresa D. Douglas,Mary J. Kennedy,Meghan E. Quirk,Sarah H. Yi,Rani H. Singh noted that there are many topics which I have not covered but which should form part of a more complete survey. Among topics which merit proper discussion I would include the re-ionisation of the intergalactic gas, the nature of the absorption line systems observed in distant quasars and their role

Accommodation

DEFER

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Armin Finkenstedt,Melanie Schranz,Sylvia B?sch,Daniela Karall,Sabine Scholl Bürgi,Christian Ensinger fault segmentation and its importance in the geometry and development of normal faults. Normal fault segments usually initiate as extension fractures in more brittle layers, with faulting occurring as the fractures propagate into the adjacent less brittle layers. Relay ramps are areas of reorientat

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Fiona M. Lewis,David J. Coman,Maryann Syrmis,Sarah Kilcoyne,Bruce E. Murdochifferent mechanisms superimposed on erosion which is a permanent process acting during the whole orogenesis..The first process acts very early in the history of mountain building, during subduction of the continental lithosphere. Early stages of collisional orogens are characterized by subduction of

拱形大橋

Curtis R. Coughlin II,Keith Hyland,Rebecca Randall,Can Ficicioglue Shumar floor thrust represents frontal fault propagation folds. Contrary to what the available graphic models suggest, the folds are plunging and are noncoaxial with the causative thrust fault (in the sense that the fold axes are oblique to the ramp-flat hinge). These features, which cannot be exp