İngilizce - Türkçe
facies teriminin İngilizce Türkçe sözlükte anlamı
- hastalık sırasında yüzün ifadesi
- dış görünüş
- fasiyes
- Kaya birikintilerinin bileşim ve oluşumlarını düzenleyen özelliklerin
- toplamı
- (Anatomi) yüz örn: facies anterior
- (Tıp) Bakınız: face
- facies occlusalis
- (Diş) (Latince) Dişin çiğneyici yüzü
- facies fossil
- fasiyes fosili
- facies of border
- sınır fasıyesi
- metamorphic facies
- metamorfik fasiyez
- albite-epidote-amphibolite facies
- albit-epidot-amfibolit fasiyesi
- amphibolite facies
- amfibolit fasiyesi
- continental facies
- (Coğrafya) karasal fasiyes
- eclogite facies
- eklojit fasiyesi
- fossil facies
- (Coğrafya) fosil fasiyesi
- glaucophane-schist facies
- glokofan-şist fasiyesi
- granulite facies
- granülit fasiyesi
- hornblende-hornfels facies
- hornblend-hornfels fasiyesi
- hornfels facies
- boynuztaşı fasiyesi
- hornfels facies
- hornfels fasiyesi
- marine facies
- (Coğrafya) denizel kayaç fasiyesi
- reef facies
- (Coğrafya) resif fasiyesi
- shallow marine facies
- (Coğrafya) sığ deniz fasiyezi
İlgili Terimler
İngilizce - İngilizce
facies teriminin İngilizce İngilizce sözlükte anlamı
- Appearance
The Chilean Amphijubula Schust. (Schuster, 1970a) which has the facies of a small Frullania and agrees with Frullania in leaf insertion and branching, has a nontiered seta with 16 epidermal cell rows surrounding 4 inner rows.
- Facial features, like an expression or complexion, typical for patients having certain diseases or conditions (e.g. costive facies)
- The assemblage of rock Refers to the appearance, characteristics and peculiarities that distinguish a rock unit from its adjacent units
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- The sum of all primary lithologic and paleontologic characteristics of sediments or sedimentary rock that are used to infer its origin and environment; the general nature of appearance of sediments or sedimentary rock produced under a given set of conditions; a distinctive group of characteristics that distinguish one group from another within a stratigraphic unit; e g contrasting river-channel facies and overbank-flood-plain facies in alluvial valley fills
- The sum total of features such as sedimentary rock type, mineral content, sedimentary structures, bedding characteristics, fossil content, etc which characterise a sediment as having been deposited in a given environment
- distinctive rock type
- Part of a rock body as differentiated from other parts by appearance or composition, often as a result of changing depositional environments Geology Ref EH
- The face of a bird, or the front of the head, excluding the bill
- The anterior part of the head; the face
- with reference to its adaptation to its environment
- a term used to refer to a distinguished part or parts of a single geologic entity
- amphibolite facies epidote amphibolite facies glaucophane schist facies granulite facies greenschist facies sedimentary facies zeolitic facies
- {i} overall appearance; facial expression characteristic of a disease (Medicine)
- Varieties
- The general aspect or habit of a species, or group of species, esp
- facies Hippocratica
- The pallid or shrunken face of someone about to die
Carew shifted his position, and once more looked anxiously at the haggard face on the pillow. It bore certain tokens which in his ignorance he fancied were characteristic of the facies hippocratica .
- amphibolite facies
- One of the major divisions of the mineral facies classification of metamorphic rocks, encompassing rocks that formed under conditions of moderate to high temperatures (950°F, or 500°C, maximum) and pressures. Less-intense temperatures and pressures form rocks of the epidote-amphibolite facies, and more-intense temperatures and pressures form rocks of the granulite facies. Amphibole, diopside, epidote, plagioclase, certain types of garnet, and wollastonite are minerals typically found in amphibolite facies rocks. They are widely distributed in Precambrian gneisses and probably formed in the deeper parts of folded mountain belts
- epidote-amphibolite facies
- One of the major divisions of the mineral facies classification of metamorphic rocks, encompassing rocks that formed under moderate temperature (500-750°F, or 250-400°C) and pressure conditions. This facies grades into the greenschist facies under less intense metamorphic conditions and into the amphibolite facies with greater temperature and pressure. Typical minerals include biotite, almandine garnet, plagioclase, epidote, and amphibole. Chlorite, muscovite, staurolite, and chloritoid may also occur
- glaucophane schist facies
- One of the major divisions of the mineral facies classification of metamorphic rocks, encompassing rocks whose peculiar mineralogy suggests that they formed under conditions of high pressure and relatively low temperature (generally less than about 662°F, or 350°C); such conditions are not typical of the normal geothermal gradient in the earth. The minerals that chiefly occur include soda amphibole (glaucophane), soda pyroxene (jadeite), garnet, lawsonite, and pumpellyite. Quartz, muscovite, chlorite, epidote, and plagioclase may also be present. Classic deposits occur in western California
- granulite facies
- One of the major divisions of the mineral facies classification of metamorphic rocks, encompassing rocks that formed under intense temperature-pressure conditions (higher than 950°F, or 500°C). The minerals found in the rocks of granulite facies include hornblende, pyroxene, biotite, garnet, calcium plagioclase, and quartz or olivine. See also amphibolite facies
- greenschist facies
- One of the major divisions of the mineral facies classification of metamorphic rocks, encompassing the rocks that formed under fairly low temperatures (480-660 °F, or 250-350 °C) and pressure conditions and usually produced by regional metamorphism. The minerals commonly found in such rocks include quartz, orthoclase, muscovite, chlorite, serpentine, talc, and epidote; carbonate minerals and amphibole (actinolite) may also be present
- sedimentary facies
- Different, but contemporaneous and juxtaposed, sedimentary rocks. Terrigenous facies are accumulations of particles eroded from older rocks and transported to the depositional site. Biogenic facies are accumulations of whole or fragmented shells and other hard parts of animals. Chemical facies result from precipitation of inorganic material from solution. The shapes and characteristics of facies may change as conditions change over time
- zeolitic facies
- One of the major divisions of the mineral facies classification of metamorphic rocks, encompassing rocks that formed at the lowest temperatures and pressures associated with regional metamorphism. Typical minerals in these facies include the zeolites, albite, and quartz