Titlebook: Backarc Basins; Tectonics and Magmat Brian Taylor Book 1995 Springer Science+Business Media New York 1995 evolution.geology.sediment.sedime

大腦

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(xué)科排名




書目名稱Backarc Basins網(wǎng)絡(luò)公開度




書目名稱Backarc Basins網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Backarc Basins被引頻次




書目名稱Backarc Basins被引頻次學(xué)科排名




書目名稱Backarc Basins年度引用




書目名稱Backarc Basins年度引用學(xué)科排名




書目名稱Backarc Basins讀者反饋




書目名稱Backarc Basins讀者反饋學(xué)科排名

世俗

珍奇

消極詞匯

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

macrophage

商議

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

MERIT

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

CRACK

社團

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

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