標(biāo)題: Titlebook: Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism, and Climate Change; Detlef Wolf,José Fernández Conference pr [打印本頁] 作者: arouse 時間: 2025-3-21 20:01
書目名稱Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism, and Climate Change影響因子(影響力)
書目名稱Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism, and Climate Change影響因子(影響力)學(xué)科排名
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書目名稱Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism, and Climate Change網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism, and Climate Change被引頻次
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書目名稱Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism, and Climate Change讀者反饋學(xué)科排名
作者: Lipohypertrophy 時間: 2025-3-21 20:19 作者: ORBIT 時間: 2025-3-22 02:56 作者: Between 時間: 2025-3-22 06:09 作者: ANN 時間: 2025-3-22 10:04
Review of Microgravity Observations at Mt. Etna: A Powerful Tool to Monitor and Study Active Volcan Etna. Two continuous gravity records are discussed: a 16-month (October 1998 to February 2000) sequence and a 48-hour (26–28 October, 2002) sequence, both from a station within a few kilometers of the volcano’s summit. The 16-month record may be the longest continuous gravity sequence ever acquired作者: Mingle 時間: 2025-3-22 15:05
An Estimate of Global Mean Sea-level Rise Inferred from Tide-gauge Measurements Using Glacial-isoste deglaciation on the tide-gauge measurements. A comparison between the observational and residual linear trends for the tide-gauge measurements shows a significant reduction of the variance and geographical variability for the latter, in particular for the formerly ice-covered regions of North Amer作者: Mingle 時間: 2025-3-22 17:27
Vertical Crustal Motion along the Mediterranean and Black Sea Coast Derived from Ocean Altimetry anese results on vertical ground motion along the Mediterranean and Black Sea coasts provide useful source data for studying, contrasting, and constraining tectonic models of the region. For example, in the eastern coast of the Adriatic Sea and in the western coast of Greece, a general subsidence is o作者: debunk 時間: 2025-3-22 21:52 作者: 騷動 時間: 2025-3-23 02:04 作者: 貪婪性 時間: 2025-3-23 07:02 作者: 別名 時間: 2025-3-23 13:02 作者: Fibroid 時間: 2025-3-23 14:57 作者: 閑聊 時間: 2025-3-23 18:10
https://doi.org/10.1007/978-3-211-75490-0um at 1890, followed by a uniform decrease until 1991, continuing to the present day at an average rate based on recent mass-balance measurements, (2) a history that is the same as the first, except for constant ice volumes prior to 1890, and (3) a history that is again the same as the first model, 作者: 溫室 時間: 2025-3-23 22:35
Erwerb und Verlust der Aktion?rsstellung Etna. Two continuous gravity records are discussed: a 16-month (October 1998 to February 2000) sequence and a 48-hour (26–28 October, 2002) sequence, both from a station within a few kilometers of the volcano’s summit. The 16-month record may be the longest continuous gravity sequence ever acquired作者: patella 時間: 2025-3-24 02:59
https://doi.org/10.1007/978-3-658-09379-2e deglaciation on the tide-gauge measurements. A comparison between the observational and residual linear trends for the tide-gauge measurements shows a significant reduction of the variance and geographical variability for the latter, in particular for the formerly ice-covered regions of North Amer作者: 增減字母法 時間: 2025-3-24 08:56 作者: SLING 時間: 2025-3-24 12:46 作者: Rebate 時間: 2025-3-24 15:28
Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism, and Climate Change作者: daredevil 時間: 2025-3-24 22:49 作者: OFF 時間: 2025-3-24 23:40 作者: 凝結(jié)劑 時間: 2025-3-25 05:48
https://doi.org/10.37307/b.978-3-503-20685-8t surface deformation and to analyze their space-time characteristics. Following the description of the main theoretical aspects of the algorithm, we present several results obtained by applying the SBAS approach in selected case studies relevant to phenomena affecting volcanic areas (Campi Flegrei 作者: goodwill 時間: 2025-3-25 09:44
https://doi.org/10.37307/b.978-3-503-21255-2al numerical methods for 2-D and 3-D glacial-isostatic adjustment (GIA) modelling have been applied recently. The present analytical approach may be used as an aid for testing more general algorithms of GIA. The propagator-matrix solution has been tested by comparing it with the analytical solution 作者: antiandrogen 時間: 2025-3-25 12:31
Stockton & Darlington Railway Company, 1858 following the last deglaciation. As a measure of this variation, sea-level indicators (SLIs) related to the RSL heights at specific past time epochs are used. For the inversion of the RSL-height change in terms of mantle viscosity, neighbouring SLIs may be grouped into an RSL diagram taken as repre作者: SEED 時間: 2025-3-25 17:45 作者: 扔掉掐死你 時間: 2025-3-25 22:11
Stockton & Darlington Railway Company, 1858an sea level (GMSL) based on Topex/Poseidon (T/P) altimetry with time-variable geoid averaged over the oceans, as observed by the GRACE (Gravity Recovery and Climate Experiment) satellite. In effect, altimetry-derived GMSL changes results from two contributions: Steric (thermal plus salinity) effect作者: insomnia 時間: 2025-3-26 02:31 作者: Palliation 時間: 2025-3-26 05:39
https://doi.org/10.1007/978-3-211-75490-0ure. Iceland offers a unique case study for GIA research, with a thinner elastic lithosphere underlain by a low-viscosity zone or asthenosphere, as opposed to regions such as Fennoscandia or North America described by a thicker lithosphere, while not necessarily featuring an asthenosphere..A lateral作者: placebo-effect 時間: 2025-3-26 12:07 作者: RENIN 時間: 2025-3-26 15:24 作者: Phagocytes 時間: 2025-3-26 17:24
https://doi.org/10.1007/978-3-658-09379-2 changes without significant deformation after the 1993 eruption. We detail the applicable data and the associated inversion techniques and models prior to calculating the appropriate stress changes. It is determined that the stress change associated with the central magmatic source produces compres作者: 丑惡 時間: 2025-3-26 23:50
Gründungsm?ngel und Gründungshaftung focused on the modeling of a single magmatic source located in the summit region of the volcano. Such models do not fit to our measurements between 2000 and 2002. A new hybrid model approach is developed consisting of an elastic-gravitational source described by a mass and energy term as well as a 作者: FOIL 時間: 2025-3-27 04:41 作者: 捐助 時間: 2025-3-27 09:16 作者: 芳香一點 時間: 2025-3-27 11:00
Detlef Wolf,José FernándezLeading experts describe major developments in geodynamics.Views on internal and surface processes of the earth作者: 脾氣暴躁的人 時間: 2025-3-27 17:11
Pageoph Topical Volumeshttp://image.papertrans.cn/d/image/264844.jpg作者: 戰(zhàn)勝 時間: 2025-3-27 18:53
https://doi.org/10.1007/978-3-7643-8417-3Climate; Geodesy; Gravity; Isostasy; Tectonics; Tide; Volcanism; economic geology作者: 為現(xiàn)場 時間: 2025-3-28 01:53
978-3-7643-8416-6Birkh?user Basel 2007作者: CURB 時間: 2025-3-28 04:07 作者: Emmenagogue 時間: 2025-3-28 07:17 作者: CHAR 時間: 2025-3-28 11:19
An Overview of the Small BAseline Subset Algorithm: A DInSAR Technique for Surface Deformation Analt surface deformation and to analyze their space-time characteristics. Following the description of the main theoretical aspects of the algorithm, we present several results obtained by applying the SBAS approach in selected case studies relevant to phenomena affecting volcanic areas (Campi Flegrei 作者: 考博 時間: 2025-3-28 16:33
Propagator-matrix Technique for the Viscoelastic Response of a Multi-layered Sphere to Surface Toroal numerical methods for 2-D and 3-D glacial-isostatic adjustment (GIA) modelling have been applied recently. The present analytical approach may be used as an aid for testing more general algorithms of GIA. The propagator-matrix solution has been tested by comparing it with the analytical solution 作者: libertine 時間: 2025-3-28 22:05 作者: 打算 時間: 2025-3-29 02:57
Shear-wave Velocity Structure around Teide Volcano: Results Using Microtremors with the SPAC Methode present an analysis of microtremor measurements recorded during the performance tests of two temporary seismic arrays installed in the eastern portion of the Teide caldera in 1994. We take advantage of recent developments of the SPAC method and use spatial cross-correlation computations to estimat作者: 脫離 時間: 2025-3-29 06:44
Steric Sea-level Variations Inferred from Combined Topex/Poseidon Altimetry and GRACE Gravimetry,an sea level (GMSL) based on Topex/Poseidon (T/P) altimetry with time-variable geoid averaged over the oceans, as observed by the GRACE (Gravity Recovery and Climate Experiment) satellite. In effect, altimetry-derived GMSL changes results from two contributions: Steric (thermal plus salinity) effect作者: Hemiparesis 時間: 2025-3-29 09:31
,Interpretation of 1992–1994 Gravity Changes around Mayon Volcano, Philippines, Using Point Sources,se of mass and pressure changes at several point sources modelled using a fast inversion process. This inversion approach attempts to fit gravity and elevation changes by combining a random search for the positions of the sources and a linear least-squares fit for the incremental mass, pressure and 作者: 修剪過的樹籬 時間: 2025-3-29 11:27
,Glacial-isostatic Adjustment and the Viscosity Structure Underlying the Vatnaj?kull Ice Cap, Icelanure. Iceland offers a unique case study for GIA research, with a thinner elastic lithosphere underlain by a low-viscosity zone or asthenosphere, as opposed to regions such as Fennoscandia or North America described by a thicker lithosphere, while not necessarily featuring an asthenosphere..A lateral作者: Acclaim 時間: 2025-3-29 19:29
Review of Microgravity Observations at Mt. Etna: A Powerful Tool to Monitor and Study Active Volcann addition to describing the methodology for acquiring and reducing gravity data from Mt. Etna, this paper provides a collection of case studies aimed at demonstrating the potential of microgravity to investigate the plumbing system of an active volcano and detect forerunners to paroxysmal volcanic 作者: concentrate 時間: 2025-3-29 23:34 作者: nepotism 時間: 2025-3-30 02:00 作者: 六邊形 時間: 2025-3-30 05:32 作者: 嚴(yán)厲譴責(zé) 時間: 2025-3-30 12:15
Vertical Crustal Motion along the Mediterranean and Black Sea Coast Derived from Ocean Altimetry antimetry (TOPEX/Poseidon and ERS-1/2) for a period of nine years (1993–2001). The TG measures the SSH relative to the ground whereas the altimetry does so with respect to the geocentric reference frame; therefore their difference would be in principle a vertical ground motion of the TG sites, though