engleski

Stratigraphic evolution of Triassic arc-backarc system in northwestern Croatia

Middle Triassic arc-related extensional tectonics in the western Tethys generated a complex pattern of intra- and backarc basins. We studied volcano-sedimentary successions of subsided continental-margin blocks (Mts. Žumberak and Ivanščica) and of dismembered incomplete ophiolite sequences interpreted as remnants of a backarc basin (Mts. Medvednica and Kalnik) in northwestern Croatia. We dated the successions with radiolarians, conodonts, foraminifers, algae, and sponges. The continental margin experienced a phase of accelerated subsidence in the Late Anisian that was approximately coincident with the onset of intermediate and acidic volcanism ; pelagic sediments with volcaniclastics accumulated atop subsided carbonate platforms. These relatively shallow basins were later infilled completely by prograding platforms in the Late Ladinian - Carnian. In the backarc basin, sea-floor spreading initiated near the Anisian-Ladinian boundary and continued into the Late Carnian. Pillow basalts were erupted and interlayered with radiolarian cherts and shales. The studied area was a part of a larger Triassic arc-backarc system preserved in the Southern Alps, Alpine-Carpathian Belt, Dinarides, and Hellenides. Volcano-sedimentary successions of Mts. Medvednica and Kalnik are relics of the Meliata-Maliak backarc basin. In comparison to other previously dated oceanic remnants of this system, the longest continuous sea-floor spreading is now documented in one restricted tectonic unit.

Arc-backarc system; Meliata-Maliak Basin; Middle Triassic; Late Triassic; Biostratigraphy; Radiolaria; Conodonts; Volcanism; Croatia

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