First find of serpentinite in the cliffs of the Heracleian Peninsula of Southwestern Crimea


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Abstract

This paper reports on the geological position and composition of serpentinite and serpentinitized peridotite, which we were the first to find in the cliffs of the southern part of the Heracleian Peninsula of Southwestern Crimea. In combination with pillow lava, gabbro, fragments of parallel dikes, and jasper, these rocks form an ophiolite association, which formerly belonged to the ancient crust of a back-arc basin that had reached the spreading stage of development.

About the authors

L. I. Demina

Department of Geology

Author for correspondence.
Email: lidem06@rambler.ru
Russian Federation, Moscow, 119991

M. Yu. Promyslova

Department of Geology

Email: lidem06@rambler.ru
Russian Federation, Moscow, 119991

N. V. Koronovskii

Department of Geology

Email: lidem06@rambler.ru
Russian Federation, Moscow, 119991

V. V. Tzarev

Department of Geology

Email: lidem06@rambler.ru
Russian Federation, Moscow, 119991

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