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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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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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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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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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Archives of Pediatrics & Adolescent Medicine, 1935
Adenoids apparently were not mentioned in the medical literature until 1867, when Wilhelm Meyer of Copenhagen described them, but there are many examples of the adenoid expression in early portraits. Almost all the Hapsburgs hang their mouths open as if they were afflicted with adenoids as well as with thin noses.
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Adenoids apparently were not mentioned in the medical literature until 1867, when Wilhelm Meyer of Copenhagen described them, but there are many examples of the adenoid expression in early portraits. Almost all the Hapsburgs hang their mouths open as if they were afflicted with adenoids as well as with thin noses.
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1971
The structure of the eastern portion of the area covered by Plate 1 can be described broadly as a homocline. Its dip is rather uniform to the east (Fig. 66), but its complexity varies drastically and discontinuously across strike. To the west it is relatively simple.
Edward Hansen, Edward Hansen
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The structure of the eastern portion of the area covered by Plate 1 can be described broadly as a homocline. Its dip is rather uniform to the east (Fig. 66), but its complexity varies drastically and discontinuously across strike. To the west it is relatively simple.
Edward Hansen, Edward Hansen
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A program in BASIC for facies-by-facies Markov chain analysis
Computers & Geosciences, 1989Abstract This paper presents a BASIC program for Markov analysis following a method proposed in 1982 by D. W. Powers and R. G. Easterling, which is appropriate for facies-by-facies analyses, in which a facies may not succeed itself. It estimates levels of significance by Powers' and Easterling's chi-square method and also by C. W.
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