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A distinctive assemblage of mafic plus ultramafic rocks, generally considered to be fragments of oceanic lithosphere that have been tectonically emplaced onto continental margins and island arcs.



a group of ultrabasic and basic intrusive (dunites, peridotites, pyroxenites, various gabbros, tonalites), effusive (primarily basalts and their tuffs), and sedimentary (pelagic oceanic deposits) rocks that are found together.

The concept of ophiolite was introduced by the Swiss scientist G. Steinmann in 1905. Ophiolites are usually associated with the manifestation of magmatism in the early stages of the formation of geosynclinal systems.

During the 1960’s and 1970’s, in connection with intensive study of the oceans, the problem of ophiolites attracted a great deal of attention. Scientists began viewing ophiolites in folded regions as relics of oceanic crust tectonically moved to the margins of the continents. Moreover, serpentinized ultrabasites are viewed as part of the mantle; gabbroids, as the “basalt layer”; and the effusive sedimentary series, as an analogue of the “first” and “second” layers of the present-day oceanic crust. A partial disruption of this sequence of rocks results from the tectonic factors that cause the development of a specific geological formation, a serpentinite rock, in which all members of the ophiolite group, as well as other rocks, are chaotically intermixed and “cemented together” by serpentinites.

Ophiolites are a common component of the earth’s linear folded regions. They are widespread in geosynclinal systems, forming within them protrusions (rock masses tectonically intruded in the solid state into the deposits covering them) or nappes thrust over the miogeosynclinal or platform sediments that overlie the continental crust. The study of ophiolites is important in discovering deposits of chromium, nickel, platinum, gold, mercury, and other ores genetically related to ophiolites, and for studying the historical development of the earth’s crust.


Peive, A. V. “Okeanicheskaia kora geologicheskogo proshlogo.” Geotektonika, 1969, no. 4.
Hess, H. H. “History of Ocean Basins.” In Buddington Volume. New York, 1962.


References in periodicals archive ?
Ophiolitic rocks are particularly abundant in these subzones, and occur in three large (>200 km by 5-20 km) well-exposed Cambrian-Early Ordovician belts (Fig.
trace elements availability to plants in ophiolitic soils.
The lead and strontium isotope geochemistry of metalliferous sediments associated with Upper Cretaceous ophiolitic rocks in Cyprus, Syria, and the Sultanate of Omen: discussion, Canadian Journal of Earth Sciences 19: 1720-24.
Dredging the ocean floor helped confirm the identities of ophiolitic sections, but Russian marine geologists and geophysicists who participated in the Deep Sea Drilling Project did not fully accept this view until 1981, when a dike complex was penetrated in Hole 504B.
The Matanzas license covers an area of 28 km 2 and together with the Quisis exploration license and the Rio Colorado application for license forms part of a 12 km long contiguous block located west of the Sechol Project and lying within the Baja Verapaz ophiolitic belt, a belt that includes major nickel deposits.
The metamorphic rocks are in tectonic contact with ophiolitic units in the northern part of the basin [13].
The concentration and outcrop of the Ophiolitic rocks complex with different erosions have caused formation of various heights and hills in different parts and this rock complex is considered the most important geological feature of the area along the Ophiolitic trend of central Iran in which numerous mineralization can be traced [1].
the spatial association with a major terrane-bounding fault zone containing interleaved ophiolitic rocks) in constraining the distribution of gold mineralization is highlighted.
The pyroxenite rock, that hosts main mineralized zones, is part of the Thetford Mine ophiolitic complex which is well known for its chromium potential.
A continental scarp extends along the northern margin of the Island and the narrow ophiolitic belt belonging to the ancient oceanic crust located to the South.