Geodynamic setting and models of the emplacement of ophiolitic allochthons in the structure of accreted island arcs of the pacific north-western framing
https://doi.org/10.32454/0016-7762-2019-2-5-11
Abstract
Based on the model of an oceanic island-arc breakup followed by accretion of rear and frontal parts of an arc to a continental margin of North-East Asia, the geodynamic nature of the ophiolites of Kamchatka and South Koryakia has been considered. The suprasubduction zone (SSZ) ophiolites originated in back-arc, fore-arc and intra-arc settings have been distinguished, and ophiolites of an ocean type have been distinguished only in one locality. The models of a SSZ ophiolites origin have been proposed. The emplacement of back-arc ophiolites has been supposed to be a result of the collapse (a closure) of a marginal basin, the emplacement of fore-arc ophiolites has been thought to be caused by their “pushing out” from a fore-arc basin, and the emplacement of the intra-arc basin ophiolites has been ascribed to a piling up of a newly formed basin crust before the beginning of the subduction. The emplacement of the ocean-type ophiolite in the front of the Olyutorsky folded structure has been attributed to a sliding accretion along the strike-slip fault movement related to the change in the motion direction of the Pacific plate 47 Ma ago.
About the Authors
V. D. ChekhovichRussian Federation
7, Pyzhevsky street, Moscow 19017.
A. N. Sukhov
Russian Federation
7, Pyzhevsky street, Moscow 19017.
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Review
For citations:
Chekhovich V.D., Sukhov A.N. Geodynamic setting and models of the emplacement of ophiolitic allochthons in the structure of accreted island arcs of the pacific north-western framing. Proceedings of higher educational establishments. Geology and Exploration. 2019;(2):5-11. (In Russ.) https://doi.org/10.32454/0016-7762-2019-2-5-11