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AAPG Bulletin, 1958 Stratigraphic facies was recognized, defined, and named by Gressly in 1838. Before the end of the nineteenth century the concept of facies became firmly established, through the works of Mojsisovics, Renevier, and Walther, as referring to the sum of lithologic and paleontologic characteristics of a sedimentary rock from which its origin and the ...
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Metamorphic Facies and Facies Series
1965Goldschmidt’s (1911) study of the contact metamorphism of the Oslo area and Eskola’s (1914) study of the regional metamorphism of the Orijarvi region revealed that well-recrystallized metamorphic rocks approached chemical equilibrium at a stage of their history and that the mineral compositions they acquired then have usually been preserved over long ...
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Shallow-marine carbonate facies and facies models
Geological Society, London, Special Publications, 1985Summary Shallow-marine carbonate sediments occur in three settings: platforms, shelves and ramps. The facies patterns and sequences in these settings are distinctive. However, one type of setting can develop into another through sedimentational or tectonic processes and, in the geologic record, intermediate cases are common.
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Facies versus Seismic Facies: Case Studies
Proceedings, 2013The presentation will touch upon the comparison of well based and seismic interpretation models on the example of two hydrocarbon fields in Pechora oil and gas basin. It shows that the latter provides much more accurate lateral distribution of reservoirs in the inter well space.
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1971
Three cross sections that radiate from Storlifjellet in the western part of the area covered by Plate 1 are shown in Fig. 26; the Indre Kam formation, consisting primarily of flagstone, is drawn in black. The sections show the general forms and relative locations of the major structural complexes in southeastern Trollheimen: Svarthammer anticline, the ...
Edward Hansen, Edward Hansen
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Three cross sections that radiate from Storlifjellet in the western part of the area covered by Plate 1 are shown in Fig. 26; the Indre Kam formation, consisting primarily of flagstone, is drawn in black. The sections show the general forms and relative locations of the major structural complexes in southeastern Trollheimen: Svarthammer anticline, the ...
Edward Hansen, Edward Hansen
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Studia Logica, 1996
The authors draw a distinction between two kinds of defeasible conditional obligation: those in which the condition merely provides a reasonable indicator of the existence of the obligation (which they term ``epistemic''), and those in which the condition provides a ``reason for the existence of the obligation'' (called ``constitutive''). They see this
Daniel Bonevac, Nicholas Asher
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The authors draw a distinction between two kinds of defeasible conditional obligation: those in which the condition merely provides a reasonable indicator of the existence of the obligation (which they term ``epistemic''), and those in which the condition provides a ``reason for the existence of the obligation'' (called ``constitutive''). They see this
Daniel Bonevac, Nicholas Asher
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The zeolite facies; an interpretation
American Journal of Science, 1961The zeolite facies, formed under conditions intermediate between diagenesis and regional metamorphism, is characterized by mineral assemblages bearing laumontite, heulandite, or analcite, together with quartz. If H 2 O and CO 2 are regarded as mobile components, these assemblages, under the same conditions, rule out the following: calcite-kaolinite ...
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1979
Publisher Summary This chapter describes the diagnosis of abnormalities of the face. The study of the face, while it cannot replace systematic examination of the body as a whole, may in many cases direct the observer's attention to the most likely field in which to find data for his diagnosis.
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Publisher Summary This chapter describes the diagnosis of abnormalities of the face. The study of the face, while it cannot replace systematic examination of the body as a whole, may in many cases direct the observer's attention to the most likely field in which to find data for his diagnosis.
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Mineralogy and Petrology, 1994
Lamprophyres are a polygenetic group of rocks that have formed by the crystallization of common magma types, including lamproites and kimberlites, under volatile-rich conditions. The term lamprophyre is considered to have no genetic significance and the recognition of a lamprophyre facies is proposed as a means of conveying the concept that some ...
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Lamprophyres are a polygenetic group of rocks that have formed by the crystallization of common magma types, including lamproites and kimberlites, under volatile-rich conditions. The term lamprophyre is considered to have no genetic significance and the recognition of a lamprophyre facies is proposed as a means of conveying the concept that some ...
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