標題: Titlebook: Backarc Basins; Tectonics and Magmat Brian Taylor Book 1995 Springer Science+Business Media New York 1995 evolution.geology.sediment.sedime [打印本頁] 作者: 大腦 時間: 2025-3-21 19:21
書目名稱Backarc Basins影響因子(影響力)
書目名稱Backarc Basins影響因子(影響力)學科排名
書目名稱Backarc Basins網絡公開度
書目名稱Backarc Basins網絡公開度學科排名
書目名稱Backarc Basins被引頻次
書目名稱Backarc Basins被引頻次學科排名
書目名稱Backarc Basins年度引用
書目名稱Backarc Basins年度引用學科排名
書目名稱Backarc Basins讀者反饋
書目名稱Backarc Basins讀者反饋學科排名
作者: 世俗 時間: 2025-3-21 21:53 作者: 珍奇 時間: 2025-3-22 03:00 作者: 消極詞匯 時間: 2025-3-22 08:09
Ryan K. Baggett,Autumn L. Stoutexhibiting strong seismic wave attenuation; it overlies the west dipping seismic zone of the Tonga Trench subduction system and is presently opening at rates as high as 1.6 cm/yr. Seaward rollback of the trench axis, coupled with upwelling high temperature mantle diapirs, is proposed as the main dri作者: macrophage 時間: 2025-3-22 09:29 作者: 商議 時間: 2025-3-22 16:26
Karen Bluth,Melissa Clepper-Faithal basin, the North Fiji Basin. This chapter reviews the structural, geophysical, geochronological, and penological data available for the New Hebrides backarc troughs (NHB AT) and discusses the significance of these structures..A diffuse horst-and-graben morphology, partly obscured in some places b作者: MERIT 時間: 2025-3-22 18:41
Ontologies and the Semantic Webarc and the West Mariana Ridge, a remnant arc. The geologic evolution of the Mariana Trough varies along strike of the basin from the initial opening phase in the north to the mature seafloor spreading phase in the central latitudes. The opening of the basin began with an initial period of stretchin作者: CRACK 時間: 2025-3-22 22:56 作者: 社團 時間: 2025-3-23 01:43
Duality and Optimality Conditionseninsula and is an example of an extensional basin formed by rifting within a continental volcanic arc. The Antarctic Peninsula is the product of at least 200 m.y. of subduction with the majority of the exposed rocks related to continental arc volcanism older than 20 Ma. Volcanism in Bransfield Stra作者: 躲債 時間: 2025-3-23 08:43 作者: Incorporate 時間: 2025-3-23 10:45
Venkataramanan Balakrishnan,Fan Wangs are summarized on the basis of updated geophysical and geological data, including swath bathymetry, gravity, magnetics, and seismic reflection profiling records as well as results from the DSDP/ODP drilling holes. It has been proposed that the Shikoku Basin was born as a rift separating the N-S tr作者: champaign 時間: 2025-3-23 15:34 作者: Irremediable 時間: 2025-3-23 20:05
W. Joost Wiersinga,Christopher W. Seymourhich is 7–8 km deep, and it contains 4 to 5+ km of technically undisturbed sedimentary fill. The oldest sedimentary rocks sampled from the basin margin are Miocene/Oligocene. Although no seafloor spreading magnetic lineations exist, we conclude that the basin has formed by backarc extension and spre作者: 自制 時間: 2025-3-24 01:30
Russell J. McCulloh M.D.,Steven M. Opal M.D.luid chemistry. These sites constitute about 20% of the known seafloor hydrothermal sites, which are dominated by those occurring at mid-ocean ridges (MORs). High-temperature hydrothermal activities in the western Pacific exclusively occur in association with submarine volcanism found either on back作者: BROTH 時間: 2025-3-24 03:16
Marcel Levi M.D., Ph.D., F.R.C.P.axis. These models are adequate in the case of backarc rifting, but a more dynamic model is needed in the case of forearc rifting. We present a revised model for backarc basin sedimentation that reflects progressive shifts in volcanism and associated depocenters through the history of a backarc basi作者: flavonoids 時間: 2025-3-24 09:42 作者: Irascible 時間: 2025-3-24 14:34 作者: 去才蔑視 時間: 2025-3-24 15:24
Book 1995ano-tectonicprocesses are best studied because of their activity. Key themes inthis volume include volcano-tectonics setting; cause and location;rift magmas; and hydrothermal activity. Researchers also presentmodels of the dynamic processes occurring in backarc basins.作者: COLIC 時間: 2025-3-24 20:48
where volcano-tectonicprocesses are best studied because of their activity. Key themes inthis volume include volcano-tectonics setting; cause and location;rift magmas; and hydrothermal activity. Researchers also presentmodels of the dynamic processes occurring in backarc basins.978-1-4613-5747-6978-1-4615-1843-3作者: 填滿 時間: 2025-3-25 01:27
e to mature spreading. Complete with numerousillustrations, each of the twelve chapters focuses on a young, activebackarc basin of the circum-Pacific-where volcano-tectonicprocesses are best studied because of their activity. Key themes inthis volume include volcano-tectonics setting; cause and loca作者: 使入迷 時間: 2025-3-25 06:59
W. Joost Wiersinga,Christopher W. Seymourstent with Miocene/Oligocene lateral fault trends between Sakhalin and Hokkaido and the strike of transverse basement ridges extending across the basin. The age of the basin may be as young as Miocene or as old as late Cretaceous. Ocean drilling is needed to establish its precise age.作者: choleretic 時間: 2025-3-25 09:16 作者: cardiac-arrest 時間: 2025-3-25 15:15
Book 1995e spreading. Complete with numerousillustrations, each of the twelve chapters focuses on a young, activebackarc basin of the circum-Pacific-where volcano-tectonicprocesses are best studied because of their activity. Key themes inthis volume include volcano-tectonics setting; cause and location;rift 作者: V洗浴 時間: 2025-3-25 18:44
Taupo Volcanic Zone and Central Volcanic Region Backarc Structures of North Island, New Zealand,wedge-shaped basin, approximately 4 m.y. old, which is defined by geophysical parameters. It corresponds to an area of low density, low-velocity volcanic rocks and anomalous seismic properties within the upper mantle. Seismic data also provide evidence for a 7.4–7.5 km/s layer at the unusually shall作者: 不透明 時間: 2025-3-25 22:03 作者: ZEST 時間: 2025-3-26 00:32
The Geology of the Lau Basin,exhibiting strong seismic wave attenuation; it overlies the west dipping seismic zone of the Tonga Trench subduction system and is presently opening at rates as high as 1.6 cm/yr. Seaward rollback of the trench axis, coupled with upwelling high temperature mantle diapirs, is proposed as the main dri作者: 充氣球 時間: 2025-3-26 04:46
The North Fiji Basin Geology, Structure, and Geodynamic Evolution, one of the most exhaustively investigated ridge axes of the world’s oceans. Today, a ridge segment more than 800 km long and 100 km wide has been fully mapped with the Sea Beam and Furono echo sounders. This ridge axis shows four main segments characterized by the same morphostructural aspect and l作者: 古代 時間: 2025-3-26 10:20 作者: Heterodoxy 時間: 2025-3-26 16:01
Geology of the Mariana Trough,arc and the West Mariana Ridge, a remnant arc. The geologic evolution of the Mariana Trough varies along strike of the basin from the initial opening phase in the north to the mature seafloor spreading phase in the central latitudes. The opening of the basin began with an initial period of stretchin作者: 范例 時間: 2025-3-26 19:19
Tectonic Framework of the East Scotia Sea,and expanded data sets now available. The East Scotia Sea floor was generated behind the east-migrating South Sandwich Trench, at a spreading center now lying along 30°W. On its western flank, lineated magnetic anomalies are identified out to at least anomaly 5 (10–11 Ma) and probably out to anomaly作者: 衍生 時間: 2025-3-26 23:57 作者: 概觀 時間: 2025-3-27 02:01
Structural and Kinematic Evolutions of the Okinawa Trough Backarc Basin,n Okinawa Trough to 30 km in the northern Okinawa Trough. The Okinawa Trough is still in a rifting stage. In the southern Okinawa Trough, magnetic anomalies are linked either to limited arc volcanic intrusions located on the northern side of the Ryukyu arc, to the axis of the main depressions where 作者: gain631 時間: 2025-3-27 08:26 作者: Senescent 時間: 2025-3-27 13:05
Opening Tectonics of the Japan Sea, Japan Sea was initiated by the extension and thinning of the proto-Japan island arc, which was situated on the margin of the Eurasian continent at ca. 30 Ma. During the extension process a large strike-slip fault was generated at the eastern margin of the proto-Japan Sea. The strike-slip movement c作者: CON 時間: 2025-3-27 16:34
Kuril (South Okhotsk) Backarc Basin,hich is 7–8 km deep, and it contains 4 to 5+ km of technically undisturbed sedimentary fill. The oldest sedimentary rocks sampled from the basin margin are Miocene/Oligocene. Although no seafloor spreading magnetic lineations exist, we conclude that the basin has formed by backarc extension and spre作者: 天真 時間: 2025-3-27 20:23
Hydrothermal Activity Related to Arc-Backarc Magmatism in the Western Pacific,luid chemistry. These sites constitute about 20% of the known seafloor hydrothermal sites, which are dominated by those occurring at mid-ocean ridges (MORs). High-temperature hydrothermal activities in the western Pacific exclusively occur in association with submarine volcanism found either on back作者: DEI 時間: 2025-3-27 22:00
Tectonic and Magmatic Controls on Backarc Basin Sedimentation,axis. These models are adequate in the case of backarc rifting, but a more dynamic model is needed in the case of forearc rifting. We present a revised model for backarc basin sedimentation that reflects progressive shifts in volcanism and associated depocenters through the history of a backarc basi作者: novelty 時間: 2025-3-28 04:41
https://doi.org/10.1007/978-3-319-07052-0 the highest on record for a backarc basin. Rates of extension in the currently active TVZ are about 7 mm/yr in the north and 18 mm/yr in the south, derived from shear strain rates varying between 0.18 and 0.5 × 10./yr shear. Subsidence rates are 1–2 mm/yr. Focal mechanisms from recent small earthqu作者: conifer 時間: 2025-3-28 09:32
Decision Making in a Convergent Societyhward toward New Zealand, penetrating the continental-oceanic arc crustal boundary. Contrary to previous models, the entire Havre Trough is now interpreted to be undergoing backarc rifting prior to true spreading, with the attendant tectonic fabric dextrally oblique to the bounding Colville and Kerm作者: Charade 時間: 2025-3-28 13:42
Ryan K. Baggett,Autumn L. Stoutgrabens that were partly sedimented and received basaltic flows. This extension and magmatism overlapped with Lau Ridge arc volcanism. The second stage of opening (about 5.5-5 Ma) was promoted by a southward-propagating rift system that formed new crust by seafloor spreading. A second propagator (ab作者: BUCK 時間: 2025-3-28 18:27 作者: 背書 時間: 2025-3-28 19:47 作者: 有其法作用 時間: 2025-3-29 01:13 作者: 擴音器 時間: 2025-3-29 06:45 作者: Conflict 時間: 2025-3-29 07:56 作者: CUMB 時間: 2025-3-29 12:23
Etienne de Klerk,Tamás Terlaky,Kees Roosone. Melt preferentially rises through the fissures and faults created by extension in the continental crust. The total amount of extension across the Okinawa Trough has been estimated from refraction and gravity data. It decreases slightly from 80 km in the southern Okinawa Trough to 74 km in the n作者: 解決 時間: 2025-3-29 17:21 作者: Bumble 時間: 2025-3-29 22:48 作者: Fibrin 時間: 2025-3-30 03:36
Russell J. McCulloh M.D.,Steven M. Opal M.D.s understandable because of small differences in parameters, such as magma signature and composition of oceanic crust, between those two systems. Frontal-arc volcanoes are proved to be the sites of vigorous high-temperature hydrothermal activity. Several investigated submarine calderas in the Izu-Bo作者: COM 時間: 2025-3-30 05:53
Marcel Levi M.D., Ph.D., F.R.C.P. black glassy volcanic fragments within coarse, sandy intervals associated with these arc systems suggest that the early rift phase of backarc basin formation is characterized by felsic (bimodal) volcanism and that volcanic centers become progressively more intermediate with time. This trend is cons作者: Migratory 時間: 2025-3-30 10:33
Taupo Volcanic Zone and Central Volcanic Region Backarc Structures of North Island, New Zealand, the highest on record for a backarc basin. Rates of extension in the currently active TVZ are about 7 mm/yr in the north and 18 mm/yr in the south, derived from shear strain rates varying between 0.18 and 0.5 × 10./yr shear. Subsidence rates are 1–2 mm/yr. Focal mechanisms from recent small earthqu作者: MUMP 時間: 2025-3-30 13:43
The Southern Havre Trough Geological Structure and Magma Petrogenesis of an Active Backarc Rift Comhward toward New Zealand, penetrating the continental-oceanic arc crustal boundary. Contrary to previous models, the entire Havre Trough is now interpreted to be undergoing backarc rifting prior to true spreading, with the attendant tectonic fabric dextrally oblique to the bounding Colville and Kerm作者: nerve-sparing 時間: 2025-3-30 19:08 作者: amyloid 時間: 2025-3-30 23:40 作者: Assignment 時間: 2025-3-31 02:56
