Konkresi (geologi): Perbedaan antara revisi
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Rescuing 1 sources and tagging 0 as dead.) #IABot (v2.0.9.2 |
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Baris 37:
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* Mozley, P.S., and Davis, J.M., 2005, ''Internal structure and mode of growth of elongate calcite concretions: Evidence for small-scale microbially induced, chemical heterogeneity in groundwater'': Geological Society of America Bulletin, v. 117, 1400-1412.
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* Scotchman, I.C., 1991, ''The geochemistry of concretions from the Kimmeridge Clay Formation of southern and eastern England'': Sedimentology. v. 38, pp.
* Thyne, G.D., and J.R. Boles, 1989, ''Isotopic evidence for origin of the Moeraki septarian concretions, New Zealand'': Journal of Sedimentary Petrology. v. 59, n. 2, pp.
* Voigt, E., 1968, ''Uber-Hiatus-Konkretion (dargestellt an Beispielen aus dem Lias)'': Geologische Rundschau. v. 58, pp.
* Wilson, M.A., 1985, ''Disturbance and ecologic succession in an Upper Ordovician cobble-dwelling hardground fauna'': Science. v. 228, pp.
* Wilson, M.A., and Taylor, P.D., 2001, ''Palaeoecology of hard substrate faunas from the Cretaceous Qahlah Formation of the Oman Mountains'': Palaeontology. v. 44, pp.
* Zaton, M., 2010, ''Hiatus concretions'': Geology Today. v. 26, pp. 186–189.
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