The story begins with a puzzle of mistaken identity. Felsic volcanic and pyroclastic rocks exposed near the village of Margečan in northern Croatia, and similar rhyolitic lavas near Kjumberk Hill in eastern Slovenia roughly 80 kilometers to the west, had long been assigned to the Southern Alpine domain—a belt of largely unmetamorphosed rocks derived from the northern margin of the Adriatic plate. Both localities sit along the Periadriatic Fault System and its eastern continuation, the Mid-Hungarian Shear Zone, colossal right-lateral strike-slip structures that slice through the eastern edge of the Alps. Yet without constraints on their burial history, the true tectonic allegiance of these volcanic rocks remained unresolved.

A team led by Matija Vukovski of the Croatian Geological Survey attacked the problem with a combination of petrography, mineral chemistry, radiometric dating, and geochemistry. Zircon crystals separated from a Margečan ignimbrite yielded a uranium-lead age of 243.8 ± 0.43 million years, while zircons from the Kjumberk rhyolite gave 242.2 ± 1.80 million years. Both ages fall squarely within the Anisian to early Ladinian stages of the Middle Triassic, confirming that the two rock suites erupted during the same brief magmatic episode, when the northern margin of Adria was stretching and thinning during the early opening of the Neotethys Ocean.

The chemistry tells a vivid story about where that magma came from. The rocks are extremely silica-rich, with silicon dioxide contents between about 69 and 82 weight percent, and they display the classic fingerprints of calc-alkaline magmatism: enrichment in large ion lithophile elements and thorium, strong depletion in niobium and tantalum, and light rare earth element patterns resembling the average upper continental crust. Neodymium isotope ratios, with initial epsilon-neodymium values between −4.42 and −5.13, point to a mantle source heavily contaminated by recycled crustal material—likely sediments and arc-derived lithologies subducted during older Paleozoic events. In short, these rhyolites were born from partial melting of a subduction-flavored mantle wedge beneath a rifted passive margin, with an assist from melting continental crust.

So far, the two localities look like twins. But the metamorphic minerals inside them diverge dramatically. Thin sections of the Margečan ignimbrite reveal phengitic muscovite—a high-silicon white mica that only grows under elevated pressure—arranged in a tectonic cleavage that cuts across the original volcanic fabric. Using the phengite geobarometer of Massonne and Schreyer, calibrated at an assumed temperature of about 300 degrees Celsius, the team calculated peak pressures of 1.1 to 1.2 gigapascals. That corresponds to burial depths of roughly 35 to 45 kilometers, far beyond anything the Southern Alps ever experienced, where Triassic strata never exceeded about 150 degrees Celsius and 0.15 gigapascals of pressure. The Margečan rocks, in other words, passed through blueschist-facies conditions—the hallmark of subduction zones.

The Kjumberk lavas, by contrast, are fresh and unmetamorphosed, entirely consistent with their placement in the Southern Alps. Two rocks with essentially identical ages, compositions, and eruptive histories thus carry utterly different tectonic biographies. The only regional event capable of producing blueschist-facies metamorphism after the Middle Triassic, the authors argue, was the Cretaceous Eoalpine subduction, during which the leading edge of the Adriatic margin was dragged beneath the overriding plate. The Austroalpine units of the Eastern Alps preserve this signature, with high- to ultrahigh-pressure metamorphism culminating around 95 million years ago. The Margečan ignimbrites, the team concludes, must belong to that Eoalpine high-pressure belt—specifically the Koralpe-Wölz nappe system—rather than to the Southern Alps.

That conclusion demands a redrawing of the map. The team proposes shifting the southern boundary of the Austroalpine units southward to the Labot and Šoštanj faults, meaning that rocks between the Pohorje Massif in Slovenia and Ivanščica Mountain in Croatia—previously assigned to the Southern Alpine domain—are instead displaced fragments of the Austroalpine nappe stack. Even the non-metamorphic Permo-Mesozoic sedimentary cover exposed at Boč and Ravna Gora mountains gets reassigned to the Austroalpine realm. The reinterpretation also neatly explains Eoalpine sericite ages reported from boreholes in the Igal unit of Hungary, a hundred kilometers east along the Mid-Hungarian Shear Zone.

How did a piece of the Alpine high-pressure belt end up in northern Croatia? The answer lies in one of the most spectacular tectonic processes in the geological record: lateral extrusion. When the Adriatic plate rammed into Europe, the thickened crust of the Eastern Alps could not simply pile upward—it squeezed sideways. The ALCAPA block, spanning the Alps, Carpathians, and Pannonian region, was extruded eastward into the Carpathian embayment during the Miocene, sliding along the Periadriatic Fault System and the Mid-Hungarian Shear Zone like a wedge of butter pushed along a table. Cumulative right-lateral offsets along these fault systems are estimated in the tens to hundreds of kilometers.

By matching the metamorphosed Margečan ignimbrites to their closest counterparts in the Eoalpine high-pressure belt—today exposed on the southern slopes of the Pohorje Massif in Slovenia—the team reconstructs a pre-extrusion position as much as 70 kilometers to the west-northwest of where the rocks sit now. Supporting evidence comes from the Oligocene to Lower Miocene sedimentary cover of the Hrvatsko Zagorje Basin north of the Šoštanj Fault, which recent work shows was transported allochthonously from the west. The implication is striking: the Austroalpine units were extruded much farther southeast than previously recognized, and the crustal stretching at the southern edge of the extruding wedge was accommodated largely by these high-offset strike-slip faults rather than by distributed extension.

Beyond reshaping the tectonic map, the study offers a practical bonus for regional geology. The Margečan and Kjumberk rocks, together with the widespread rhyolitic Pietra Verde tuffs scattered across the Adriatic realm, likely represent source eruptions for that distinctive green tuff marker horizon, which geologists use to correlate Triassic successions from the Southern Alps to the External Dinarides. But the deeper lesson is methodological: in a collision zone where three great orogenic domains converge, lithology alone cannot tell you where a rock belongs. Only the pressure-temperature path etched into its minerals—here, a single high-silicon mica—can reveal whether a quiet hillside in Croatia once rode a subducting slab into the deep crust and then surfed a network of continental faults to its present home.

Subject of Research: Middle Triassic ignimbrites recording Eoalpine high-pressure metamorphism and lateral extrusion of Austroalpine units at the Alps–Dinarides transition

Article Title: Middle Triassic ignimbrites as markers of Eoalpine high-pressure metamorphism and large-scale lateral extrusion of Adria derived units at the edge of the European Alps

Article References: Vukovski, M., Slovenec, D., Belak, M., Šegvić, B., Mišur, I., Smirčić, D., Horvat, M., Kukoč, D., Grgasović, T., & Slivšek, G. (2026). Middle Triassic ignimbrites as markers of Eoalpine high-pressure metamorphism and large-scale lateral extrusion of Adria derived units at the edge of the European Alps. Solid Earth, 17(7), 895-922. https://doi.org/10.5194/se-17-895-2026

Image Credits: AI Generated

DOI: 10.5194/se-17-895-2026

Keywords: ignimbrites, Eoalpine metamorphism, blueschist facies, phengite geobarometry, U-Pb zircon dating, Adria plate, Austroalpine units, Southern Alps, lateral extrusion, Periadriatic Fault System, Triassic volcanism, Alps–Dinarides transition