Results 141 to 150 of about 1,578 (175)
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PALAIOS, 1994
The nature and distribution of trace-fossil and microbenthic assemblages in Tethyan hemipelagic carbonates and marks of the Podzamcze Formation (Bajocian, Pieniny Klippen Belt) are studied. These analyses allow the identification of (1) recurring Planolites-Chondrites, Planolites-Chondrites-Zoophycos/Teichichnus and Chondrites ichno-assemblages, and (2)
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The nature and distribution of trace-fossil and microbenthic assemblages in Tethyan hemipelagic carbonates and marks of the Podzamcze Formation (Bajocian, Pieniny Klippen Belt) are studied. These analyses allow the identification of (1) recurring Planolites-Chondrites, Planolites-Chondrites-Zoophycos/Teichichnus and Chondrites ichno-assemblages, and (2)
openaire +1 more source
Spectroscopic identification of water emission from a main-belt comet
Nature, 2023Michael S Kelley +2 more
exaly
2011
Brittle structural analyses of outcrops in the Outer West Carpathian (OWC) flysch units of Southern Moraviaand Northwest Slovakia distinguished four different deformations (DF1, DF2, DF3, DF4; see Beidinger et al., thisvolume) from Paleocene to Upper Miocene times.
Beidinger, Andreas +3 more
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Brittle structural analyses of outcrops in the Outer West Carpathian (OWC) flysch units of Southern Moraviaand Northwest Slovakia distinguished four different deformations (DF1, DF2, DF3, DF4; see Beidinger et al., thisvolume) from Paleocene to Upper Miocene times.
Beidinger, Andreas +3 more
openaire +1 more source

