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Titlebook: Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites; Contributions to a S R. L. M. Vissers,A. Nicolas Conference proceedings

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發(fā)表于 2025-3-21 17:57:25 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites
副標(biāo)題Contributions to a S
編輯R. L. M. Vissers,A. Nicolas
視頻videohttp://file.papertrans.cn/624/623446/623446.mp4
叢書名稱Petrology and Structural Geology
圖書封面Titlebook: Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites; Contributions to a S R. L. M. Vissers,A. Nicolas Conference proceedings
描述This volume follows a Specialized Symposium on "Mantle denudation in slow spreading ridges and in ophiolites", held at the XII EUG Meeting in Strasbourg, spring 1993. During the meeting it was felt that the contribu- tions to the Symposium justified a volume presenting its main scientific achievements. The present title of the volume shows that the center of inter- est has slightly shifted with respect to the initial objective: in order to under- stand the processes involved in accretion taking place at oceanic ridges, it is crucial to study the interaction between uppermost mantle and lower crust. The approach favored here is that of petrological and structural analysis of oceanic rocks in present-day oceanic ridges combined with similar studies in ophiolites. Rock specimen collected by submersibles or dredge hauls in oceanic ridge environments provide a "ground truth". However, except for areas such as the MARK (Mid-Atlantic Ridge ne ar Kane fracture zone) where, thanks to multiple submersible dives, the local geology is known with aprecision even better than in many onshore ophiolites, mutual rela- tionships between uppermost mantle and lower crust are poorly known. In contrast,
出版日期Conference proceedings 1995
關(guān)鍵詞Deformation; Mafic; Ocean; dike; marine; structural geology
版次1
doihttps://doi.org/10.1007/978-94-015-8585-9
isbn_softcover978-90-481-4557-7
isbn_ebook978-94-015-8585-9Series ISSN 0924-1957
issn_series 0924-1957
copyrightSpringer Science+Business Media Dordrecht 1995
The information of publication is updating

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An Ultramafic Lift at the Mid-Atlantic Ridge: Successive Stages of Magmatism in Serpentinized Peridoalong the Mid-Atlantic Ridge to constrain a model for the building of the lower crust at magma-starved ocean ridges. This model involves successive stages of magmatism within mantle rocks that are rising up from the asthenosphere, and throughout the axial lithosphere, to ultimately form seafloor exp
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Gabbroic Dikelets in Serpentinized Peridotites from the Mid-Atlantic Ridge at 23°20’Nes show evidence of minor magmatic intrusion that produced millimetre to centimetre thick gabbroic dikelets. The nature of the intruding magma and the time relationships between intrusion events and tectonic evolution of the host peridotites is inferred from the mineralogy and textural features of v
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Mafic and Ultramafic Intrusions into Upper Mantle Peridotites from Fast Spreading Centers of the Eased by the R.V. Sonne. One of these areas is located on the western boundary of the microplate along the West Rift zone near 24°13′S and 115°41′W, and is associated with a small transform fault called Terevaka. The other area consists of a depression called the Pito Deep located at the northern tip o
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A Detailed Study of Mantle Flow away from Diapirs in the Oman Ophioliteop of mantle diapirs. In the Oman ophiolite, however, the shear direction inversion is not systematically developed at the same level in the ophiolite sequence. In particular, in the vicinity of mantle diapirs, the uppermost mantle forced flow diverging from the diapir has a clear outward (top away
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