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Methods of compaction reconstruction in carbonate sediments
Języki publikacji
Abstrakty
W artykule przedstawiono wybrane metody badań nad stopniem kompakcji osadów węglanowych, umożliwiając ich weryfikację oraz znaczenie. Ogólnie, proces kompakcji można podzielić na kompakcję mechaniczną (fizyczną) i chemiczną. Szacowanie stopnia kompakcji jest przydatne m. in. do rekonstrukcji pierwotnej miąższości osadów. Rekonstruując pierwotną miąższość osadów, stosuje się różne wskaźniki i metody. Dokonuje się tego m. in. w oparciu o obserwacje makroskopowe, mikroskopowe oraz pod mikroskopem skaningowym. Makroskopowo stopień kompakcji ocenia się sumując miąższości osadu rozpuszczonego wskutek stylolizacji. Mikroskopowo ocenia się stopień deformacji skamieniałości i ziaren, za pomocą mikroskopu elektronowego ocenia się zniekształcenia palynomorpha.
This article presents exemplary researches on the degree of compaction on carbonate sediments, allowing them to discuss their significance. Generally, compactional processes may be divided into two categories: mechanical (physical) and chemical. Knowledge about the degree of compaction is helpful e. g. in reconstruction of the primary thickness. The degree of compaction is measured by several methods and indicators. To estimate the degree of compaction, macroscopic and microscopic examinations as well as a scanning electron microscope (SEM) are applied. Macroscopically, the degree of compaction is calculated by summing the thicknesses of sediments that had been dissolved by the stylolization processes. Microscopically, the degree of compaction is estimated on the base of observations on fossils and grains deformations and the SEM method- palynomorpha deformations.
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
35--43
Opis fizyczny
Bibliogr. 36 poz., rys.
Twórcy
autor
- Akademia Górniczo-Hutnicza, Wydział Geologii, Geofizyki i Ochrony Środowiska, 30-059 Kraków, al. Mickiewicza 30, kochman@geol.agh.edu.pl
Bibliografia
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- 5. BUDD DA, PARK A.J, ORTOLEVA P.J., 2002 - Diagenesis and compaction of limestone associated with early burial and meteoric and sea water inflations: a Basin RTM simulation of the Florida carbonate platform, Geological Society America, 34, 334-335 (abstract).
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- 8. CLARI P., MARTIRE L., 1996 -Interplay of cementation, me. chanical compaction, and chemical compaction in nodular limestones of the Rosso Ammonitico Veronese (middle-upper Jurassic, northeastem Italy), J. Sedim. Reasearch, 66, 447-458.
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- 18. KATSMAN R., AHARONOW E., 2006 - A study of compaction bands originating from crack, notches, and compacted defects, Journal of Structural Geology, 28, 508--518.
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- 20. MARTIRE L., CLARI P., 1994 - Evaluation of sedimentation rates in Jurassic-Cretaceous pelagic facies of the Trento Plateau: relevance of discontinuities and comaction, Giomale di Geologia, 56/2, 193-209.
- 21. MATYJA B.A, WIERZBOWSKI A., 1996 - Sea- bottom relief and bathymetry of Late Jurassic sponge megafacies in Central Poland, Advances in Jurassic Research, GeoResearch Forum, 1-2.
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- 31. TONDI E., ANTONELLlNI M., AYDIN A., MARCHEGIANI L., CELLO G., 2006 - The role of deformation bands, stylolites and sheared stylolites in fault development in carbonate grainstones of Majella Mountain, Italy, Journal of Structural Geology, 28, 376-391.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BPZ3-0018-0006