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- W1579864871 endingPage "218" @default.
- W1579864871 startingPage "177" @default.
- W1579864871 abstract "Major faulted escarpments on the seafloor provide tectonic windows into oceanic crust and upper mantle. Direct observations in these settings reveal that the spatial arrangement, internal structure, and contacts between major rock units are significantly more complex than commonly anticipated on the basis of seismic studies and ophiolite analogs. From this perspective, a stratiform, ophiolite-like sequence of rock units, including basaltic volcanic rocks, sheeted diabase dike complex, isotropic and layered gabbroic and ultramafic rocks over upper mantle peridotites-all separated by generally horizontal contacts, may be much less common in the oceanic lithosphere than generally thought. Conversely, documented examples of large outcrop areas (tens of kilometers across) that lack the ophiolite-like sequence or that contain structures that do not conform to the ophiolite model call into question the basic assumptions made in the reconstruction and interpretation of ophiolite complexes. Historically, the stratiform ophiolite architecture has been the basis for inferences of the interaction between tectonism and magmatism at mid-ocean ridge spreading centers." @default.
- W1579864871 created "2016-06-24" @default.
- W1579864871 creator A5051732826 @default.
- W1579864871 date "2013-03-18" @default.
- W1579864871 modified "2023-10-17" @default.
- W1579864871 title "Internal Structure of Oceanic Lithosphere: A Perspective from Tectonic Windows" @default.
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