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- W2314343070 abstract "Uppermost 160 metres in the cored borehole Tdp-1/84 Trobni Dol, mainly consist of volcaniclastic sediments, deposited entirely in a marine environment. Two phases of volcanic activity were recognised, the second one producing huge amounts of pyroclastic material of rhyolitic composition, transported in a submarine pyroclastic flow and settled as an over 107 m thick ignimbrite deposit. After termination of explosive volcanic activity, sedimentation of fossiliferous marine mudstone Sivica continued, and immediately above the ignimbrite it contains a few cm thick layer of rhyolite-mudstone peperite. Peperite formed when magma intruded into a water-saturated muddy sediment, desintegrated into hyaloclasts owing to chill-and-quench processes, and finally, intermixed with the sediment. Overlying syn-eruptive resedimented volcaniclastics were deposited after ceassation of volcanic activity, with normal marine transport and sedimentation agents." @default.
- W2314343070 created "2016-06-24" @default.
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- W2314343070 date "1998-12-30" @default.
- W2314343070 modified "2023-09-26" @default.
- W2314343070 title "Volcaniclastic Rocks in Borehole Tdp-1/84 Trobni Dol, E Slovenia" @default.
- W2314343070 doi "https://doi.org/10.5474/geologija.1998.009" @default.
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