標題: Titlebook: Geodynamics of the Latin American Pacific Margin; William L. Bandy,Juanjo Da?obeitia,Rafael Bartolom Book Feb 20171st edition Springer Int [打印本頁] 作者: energy 時間: 2025-3-21 20:06
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書目名稱Geodynamics of the Latin American Pacific Margin影響因子(影響力)學科排名
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書目名稱Geodynamics of the Latin American Pacific Margin網(wǎng)絡公開度學科排名
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書目名稱Geodynamics of the Latin American Pacific Margin讀者反饋
書目名稱Geodynamics of the Latin American Pacific Margin讀者反饋學科排名
作者: 并置 時間: 2025-3-21 20:15
Foreshock Patterns Preceding Great Earthquakes in the Subduction Zone of Chile,al foreshock sequences has shown that foreshocks are characterized by distinct 3D patterns: their epicenters move towards the main shock epicenter, event count accelerates, and .-value drops. However, these space–time-size patterns were verified so far only in a very few individual cases mainly due 作者: ineffectual 時間: 2025-3-22 03:46
Analysis of the Aeromagnetic Anomalies of the Auca Mahuida Volcano, Patagonia, Argentina,le geological information. Most of the detected magnetic anomalies have a dipolar structure opposite to that of the present geomagnetic field. According to the available geochronological data and paleomagnetic measurements, the source bodies of Auca Mahuida mainly emplaced in the Matuyama reverse po作者: 針葉 時間: 2025-3-22 07:22 作者: Ibd810 時間: 2025-3-22 09:41 作者: conjunctivitis 時間: 2025-3-22 15:39
Three-Dimensional Thermal Model of the Costa Rica-Nicaragua Subduction Zone,uake seismogenic zone and volcanic arc magmatism. Here, we present the first three-dimensional (3D), steady-state kinematic-dynamic thermal model for the Costa Rica-Nicaragua subduction zone. The model consists of the subducting Cocos plate, the overriding Caribbean Plate, and a viscous mantle wedge作者: conjunctivitis 時間: 2025-3-22 20:41
,Kinematic 3-D Retro-Modeling of an Orogenic Bend in the South Limón Fold-and-Thrust Belt, Eastern Cnes and is therefore a natural laboratory for the analysis of curved orogens. The analysis of curved fold-and-thrust belts is a challenge because of the varying structural orientations within the belt. Based on seismic reflection lines, we created a 3-D subsurface model containing three major thrust作者: 描述 時間: 2025-3-22 22:44
,Low Angle Contact Between the Oaxaca and Juárez Terranes Deduced From Magnetotelluric Data,cognized tectonic features at upper to mid-crustal depths. Our results support the hypotheses that the upper crust of the Oaxaca terrane is a residual?~20?km thick crust composed by an?~10?km thick faulted crustal upper layer and an?~10?km thick hydrated and/or mineralized layer. Oaxaca basement ove作者: 陶器 時間: 2025-3-23 02:17
Seismic Anisotropy and Mantle Flow Driven by the Cocos Slab Under Southern Mexico,rn Mexico starting at the coast of the Pacific Ocean and running north toward the Gulf of Mexico. In this segment of the Middle America Trench the oceanic Cocos plate subducts under the continental North American plate. The active volcanic arc is located at the southern end of the Trans-Mexican Volc作者: Thymus 時間: 2025-3-23 05:53
Toroidal, Counter-Toroidal, and Upwelling Flow in the Mantle Wedge of the Rivera and Cocos Plates: bduction zone. The scaled model consists of a transparent tank filled with corn syrup and housing two conveyor belts made of polyethylene strips. One of the strips dips 60° and moves at a velocity of 30?mm/min simulating the Rivera plate. The other one dips 45°, moves at 90?mm/min simulating the sub作者: 北極熊 時間: 2025-3-23 10:45
Active Crustal Faults in the Forearc Region, Guerrero Sector of the Mexican Subduction Zone,iated with the occurrence of subduction earthquakes and shallow earthquakes of the overriding plate. We present the results of geomorphic, structural, and fault kinematic analyses conducted on the convergent margin between the Cocos plate and the forearc region of the overriding North American plate作者: 顯而易見 時間: 2025-3-23 15:10 作者: Ophthalmologist 時間: 2025-3-23 18:06 作者: Exposition 時間: 2025-3-24 02:06 作者: ethereal 時間: 2025-3-24 02:31 作者: entitle 時間: 2025-3-24 07:42 作者: indenture 時間: 2025-3-24 11:06 作者: 愛社交 時間: 2025-3-24 15:10
https://doi.org/10.1007/978-3-0348-4170-2le geological information. Most of the detected magnetic anomalies have a dipolar structure opposite to that of the present geomagnetic field. According to the available geochronological data and paleomagnetic measurements, the source bodies of Auca Mahuida mainly emplaced in the Matuyama reverse po作者: omnibus 時間: 2025-3-24 21:04 作者: 低三下四之人 時間: 2025-3-25 02:54 作者: 開始沒有 時間: 2025-3-25 04:16
https://doi.org/10.1007/978-3-642-52658-9uake seismogenic zone and volcanic arc magmatism. Here, we present the first three-dimensional (3D), steady-state kinematic-dynamic thermal model for the Costa Rica-Nicaragua subduction zone. The model consists of the subducting Cocos plate, the overriding Caribbean Plate, and a viscous mantle wedge作者: Canyon 時間: 2025-3-25 09:32
https://doi.org/10.1007/978-3-642-86315-8nes and is therefore a natural laboratory for the analysis of curved orogens. The analysis of curved fold-and-thrust belts is a challenge because of the varying structural orientations within the belt. Based on seismic reflection lines, we created a 3-D subsurface model containing three major thrust作者: 分離 時間: 2025-3-25 15:16
https://doi.org/10.1007/978-3-642-52656-5cognized tectonic features at upper to mid-crustal depths. Our results support the hypotheses that the upper crust of the Oaxaca terrane is a residual?~20?km thick crust composed by an?~10?km thick faulted crustal upper layer and an?~10?km thick hydrated and/or mineralized layer. Oaxaca basement ove作者: Chipmunk 時間: 2025-3-25 16:59
Die Eisenmetalle (Stahl und Eisen)rn Mexico starting at the coast of the Pacific Ocean and running north toward the Gulf of Mexico. In this segment of the Middle America Trench the oceanic Cocos plate subducts under the continental North American plate. The active volcanic arc is located at the southern end of the Trans-Mexican Volc作者: LEERY 時間: 2025-3-25 22:41 作者: Lyme-disease 時間: 2025-3-26 03:52
R. Durrer,G. Volkert,W. Dautzenbergiated with the occurrence of subduction earthquakes and shallow earthquakes of the overriding plate. We present the results of geomorphic, structural, and fault kinematic analyses conducted on the convergent margin between the Cocos plate and the forearc region of the overriding North American plate作者: 碎石 時間: 2025-3-26 06:35
Zur Morphologie des Sittlichen,failure stress changes for the six major slow slip events (SSEs) that occurred below Mexico between late 2005 and mid-2011. Slip distributions are the first to be estimated from all continuous GPS data in central and southern Mexico, which better resolves slow slip in space and time than was previou作者: 終端 時間: 2025-3-26 10:05 作者: Encephalitis 時間: 2025-3-26 15:07 作者: 通便 時間: 2025-3-26 16:53
978-3-319-51528-1Springer International Publishing AG 2017作者: nonplus 時間: 2025-3-26 22:53 作者: 招人嫉妒 時間: 2025-3-27 01:30 作者: 發(fā)起 時間: 2025-3-27 05:30
2504-3625 contributed to the collection..Studies illustrate the vast .Geodynamics of the Latin American Pacific Margin presents a collection of 22 studies by a multinational group of investigators whose common interest is to better understand the complex geodynamic processes occurring along the Pacific margi作者: 性學院 時間: 2025-3-27 11:46 作者: BAIT 時間: 2025-3-27 15:52 作者: 和平主義 時間: 2025-3-27 21:43
,Low Angle Contact Between the Oaxaca and Juárez Terranes Deduced From Magnetotelluric Data,forces may contribute to uplift because it is largely uncompensated. In the Sierra Madre del Sur, closer to the coast, uplift is facilitated by slab-dehydration driven buoyancy. Both gravity and resistivity models are consistent with a thinned upper crust in the northeast end of the profile.作者: 忘川河 時間: 2025-3-28 00:19
P. H?lemann,R. Hasselmann,G. Dixerprint and amphibolite-eclogite transition, respectively. (4) The evidences that document ridge-jump events and associated microplate individualization during subduction of the SCR1 and SCR-1 segments: the Chonos and Cabo Elena microplates, respectively. The ridge-jump process associated with the o作者: harrow 時間: 2025-3-28 02:45
Textilforschungsanstalt Krefeldomains. The pattern recognition in one domain was independent of the pattern recognition in another domain. We found and verified with two independent catalogue data sets (CSN, IPOC) that within a critical area of ca. 65?km from the main shock epicenter, the 2014 event was preceded by distinct fores作者: 圍巾 時間: 2025-3-28 08:22
https://doi.org/10.1007/978-3-0348-4170-2trikes and source geometries indicate an emplacement of intrusive bodies controlled by the regional faults affecting the Auca Mahuida basement and the sedimentary successions of the Neuquén basin. Magma upraised along these faults and fractures feeding the volcanic activity and subsequently crystall作者: 膽小懦夫 時間: 2025-3-28 14:18 作者: HAWK 時間: 2025-3-28 15:38 作者: Lime石灰 時間: 2025-3-28 21:30
https://doi.org/10.1007/978-3-642-52658-9s of up to 80?°C in the subducting slab and mantle wedge at the volcanic arc and backarc. The 3D effects do not strongly alter the shallow (<35?km) thermal structure of the subduction zone. The models predict that the megathrust seismogenic zone width decreases from ~100?km below Costa Rica to just 作者: 包庇 時間: 2025-3-28 23:58 作者: Congregate 時間: 2025-3-29 06:57
Die Eisenmetalle (Stahl und Eisen)ermined using . phases are oriented NE–SW, in the same direction as the relative motion between the Cocos and North American plates, and are approximately perpendicular to the trench. Physical conditions in the subslab mantle are consistent with the existence of A-type olivine and consequently entra作者: 一大塊 時間: 2025-3-29 10:01
https://doi.org/10.1007/978-3-662-34062-2 pressure gradient associated with the down-dip differential-motion of the slabs. Similarly, low pressure generated by the fast-moving Cocos plate creates a shallow counter-toroidal flow in the uppermost 100?km of the mantle wedge. The flow draws mantle beneath the western Trans-Mexican Volcanic Bel作者: 含水層 時間: 2025-3-29 12:27
R. Durrer,G. Volkert,W. Dautzenbergasins, GPS measurements, and obliquity of plate convergence along the Cocos subduction zone in the Guerrero sector suggest the activity of sub-latitudinal left-lateral strike-slip faults. Notably, the regional left-lateral strike-slip fault that offsets the Papagayo River near the town of La Venta n作者: Chemotherapy 時間: 2025-3-29 16:31 作者: Bridle 時間: 2025-3-29 23:47 作者: mydriatic 時間: 2025-3-30 01:22 作者: bacteria 時間: 2025-3-30 05:18 作者: Enliven 時間: 2025-3-30 09:00
Foreshock Patterns Preceding Great Earthquakes in the Subduction Zone of Chile,omains. The pattern recognition in one domain was independent of the pattern recognition in another domain. We found and verified with two independent catalogue data sets (CSN, IPOC) that within a critical area of ca. 65?km from the main shock epicenter, the 2014 event was preceded by distinct fores作者: Expiration 時間: 2025-3-30 13:32
Analysis of the Aeromagnetic Anomalies of the Auca Mahuida Volcano, Patagonia, Argentina,trikes and source geometries indicate an emplacement of intrusive bodies controlled by the regional faults affecting the Auca Mahuida basement and the sedimentary successions of the Neuquén basin. Magma upraised along these faults and fractures feeding the volcanic activity and subsequently crystall作者: Forage飼料 時間: 2025-3-30 20:22 作者: Psychogenic 時間: 2025-3-30 20:47
The 10 April 2014 Nicaraguan Crustal Earthquake: Evidence of Complex Deformation of the Central Ameplane with the same orientation as the aftershock sequence. For an earthquake of this magnitude, seismic scaling relations between fault length and magnitude predict a sub-surface fault length of approximately 16?km. This length is in good agreement with the extent of the fault defined by the afters作者: 違抗 時間: 2025-3-31 01:14
Three-Dimensional Thermal Model of the Costa Rica-Nicaragua Subduction Zone,s of up to 80?°C in the subducting slab and mantle wedge at the volcanic arc and backarc. The 3D effects do not strongly alter the shallow (<35?km) thermal structure of the subduction zone. The models predict that the megathrust seismogenic zone width decreases from ~100?km below Costa Rica to just 作者: 收藏品 時間: 2025-3-31 08:36
