Tagasi otsingusse
Kazmierczak & Pszczólkowski, 1968
Synsedimentary discontinuities in the Lower Kimmeridgian of the Holy Cross Mts
Kazmierczak, J., Pszczólkowski, A.
Aasta | 1968 |
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Ajakiri | Acta Geologica Polonica |
Köide | 18 |
Number | 3 |
Leheküljed | 587-612 |
Tüüp | artikkel ajakirjas |
Keel | poola |
Id | 10304 |
Abstrakt
Results of investigations of the discontinuity surfaces in the Lower Kimmeridgian limestones and marls of the south-western Mesozoic margin of the Holy Cross Mts. are reported. Sedimentary discontinuities, indicated by surfaces representing the various stages of the consolidation of the deposit during non-deposition, have been distinguished on the basis of paleoecologlcal and lithological analyses. The evidence now available suggests a very shallow zone of the formation of these surfaces in high-energy marine environment. Breaks in sedimentation were probably connected here with intermittently retarded subsidence.
Viimati muudetud: 27.1.2021