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U radu objavljenom u \u010dasopisu Journal of the Geological Society prezentirani su najnoviji biostratigrafski i geokemijski podaci iz ofiolitnog melan\u017ea Ivan\u0161\u010dice. Blokovi bazalta i ro\u017enjaka prepoznati su kao ostaci nekada\u0161nje oceanske kore i na njoj istalo\u017eenih dubokomorskih sedimenata sjeverozapadnog dijela Neotetis oceana. Bazaltne stijene geokemijski su okarakterizirane kao E-MORB \u010diji nastanak upu\u0107uje na formiranje srednjeoceanskog grebena i po\u010detak oceanizacije. Najstarije zajednice radiolarija iz ro\u017enjaka u kontaktu s bazaltima karakteristi\u010dne su za srednji trijas (kasni anizik \u2013 rani ladinik). Dobivene starosti korelativne su s najstarijim biostratigrafskim datacijama oceanske kore sjeverozapadnog Neotetis oceana sa\u010duvanim u ofiolitnim kompleksima Alpsko \u2013 Dinaridsko \u2013 Helenidskog pojasa, \u0161to upu\u0107uje na zajedni\u010dko porijeklo iz jedinstvenog oceanskog prostora koji se nalazio isto\u010dno od kontinentalnog ruba adrijske mikroplo\u010de. \u00a0<\/p>\n
Objavljeni podaci dio su istra\u017eivanja provedenog u sklopu HRZZ projekta GOST (IP-2019-04-3824) Hrvatske zaklade za znanost.<\/p>\n