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  1. Pseudostratigraphy and definition

    The stratigraphic-like sequence observed in ophiolites corresponds to the lithosphere-forming processes at mid-oceanic ridges. From top to bottom, the layers in the sequence are:
    • … See more

    Formation and emplacement

    Ophiolites have been identified in most of the world's orogenic belts. However, two components of ophiolite formation are under debate: the origin of the sequence and the mechanism for ophiolite emplaceme… See more

    Research

    Scientists have drilled only about 1.5 km into the 6- to 7-kilometer-thick oceanic crust, so scientific understanding of oceanic crust comes largely from comparing ophiolite structure to seismic soundings of in situ ocea… See more

    Groups and assemblages

    Ophiolites are common in orogenic belts of Mesozoic age, like those formed by the closure of the Tethys Ocean. Ophiolites in Archean and Paleoproterozoic domains are rare.
    Most ophiol… See more

     
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  2. An ophiolite is a section of Earth's oceanic crust and the underlying upper mantle that has been uplifted and exposed, and often emplaced onto continental crustal rocks. The Greek word ὄφις, ophis (snake) is found in the name of ophiolites, because of the superficial texture of some of them. Serpentinite especially evokes a snakeskin.
    en.wikipedia.org/wiki/Ophiolite
    An ophiolite is a section of the Earth's oceanic crust. The underlying upper mantle has been uplifted and exposed above sea level. The rocks which make up ophiolites are an altered form of basalt. The rocks are often green. They are found in the mountain belts such as the Alps or the Himalayas.
    simple.wikipedia.org/wiki/Ophiolite
    Ophiolites are sequences of mafic to ultramafic rock generally believed to represent ancient oceanic lithosphere. They are distributed all across the world being all of them located at present or past orogenic belts, sites of mountain building processes.
    en.wikipedia.org/wiki/List_of_ophiolites
    It is one of the world's largest and best-exposed segments of oceanic crust, made of volcanic rocks and ultramafic rocks from the Earth's upper mantle that was overthrust onto the continental crust. This ophiolite provides insight into the dynamics of oceanic crust formation and the tectonic processes involved in the creation of ocean basins.
    en.wikipedia.org/wiki/Samail_Ophiolite
     
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