Nghĩa của từ facies bằng Tiếng Việt

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Đặt câu có từ "facies"

Dưới đây là những mẫu câu có chứa từ "facies", trong bộ từ điển Từ điển Y Khoa Anh - Việt. Chúng ta có thể tham khảo những mẫu câu này để đặt câu trong tình huống cần đặt câu với từ facies, hoặc tham khảo ngữ cảnh sử dụng từ facies trong bộ từ điển Từ điển Y Khoa Anh - Việt

1. The following age sequence of metamorphic facies of alpine age is reported: (1) glaucophane-schist facies; (2) albite-epidote-amphibolite facies; (S) almandine-amphibolite facies.

2. Amphibolite facies is usually a product of Barrovian Facies Sequence or advanced Abukuma Facies Sequence metamorphic trajectories

3. Volcanic eruption facies and flooding facies are extensively developed in the Sihetun area, west Liaoning.

4. This provides precedent for facies - controlled modeling of complex block reservoirs of fluvial facies.

5. Amphibolite facies is a result of continuing burial and thermal heating after Greenschist facies is exceeded.

6. 20 This provides precedent for facies - controlled modeling of complex block reservoirs of fluvial facies.

7. Examples include Arenaceous and argillaceous facies

8. You may call my facies whimsical.

9. Sample from the Ariegite facies (his sample R243)

10. According to modern facies distributions the Roßfeld Fm. can be interpreted as a prograding deep sea channel facies.

11. Many algae are quantitatively significant constituents in various facies and some forms functioned as framebuilders in reef facies.

12. Greenschist facies minerals are mostly albite, epidote, chlorite, calcite, and quartz, whereas amphibolite facies minerals are predominantly hornblende, plagioclase (andesine), and epidote.

13. This was initially metamorphosed in the almandine-amphibolite facies before profound ruptural or cataclastic and crystalloblastic deformation evolved mylonitic rocks in the green schist facies.

14. Examples are given of “facies-nappes” and of nappes having been cut out of primary facies-basins in oblique angles.

15. Distributary plain facies sands body: . Meandering sands micro-facies, which represents large low sinuosity meandering disposition, and the channel sands is very large.

16. Regional metamorphism produced parageneses of the almandine amphibolite facies.

17. Dynamical metamorphism under greenschist facies is the condition of mineralizing enrichment.

18. Between the autochthonous reef and the detritus facies a near-reef detritus-facies can be observed, which is characterized by abundant encrusting algae acting as sedimentbinding organisms.

19. The shoal ( or bank ) and shoal facies are important types of carbonate deposits.

20. mouth and limnetic, littoral, weathered continental drift bed and flood deposit facies. ...

21. Thermodynamic activity - traces acted as the regional metamorphic facies and its belts.

22. The Thanetian pebbles indicate a coral/red algae reef complex with differing facies areas.

23. The facies of a modern beach is probably seldom preserved in the geological record.

24. The skin of the face and forehead becomesthickened and corrugated, known as "leonine facies."

25. The reservoir physical property were primarily dominated by sedimentary facies 、 corrosion and dolomization.

26. Epidote–amphibolite facies include the critical assemblage calcic pyroxene + calcic amphibole (magnesiohornblende and pargasite) + muscovite + garnet + plagioclase + epidote ± quartz, whereas greenschist facies is defined by the assemblage actinolite + albitic plagioclase + epidote + chlorite.

27. Eskola defined its "Amphibolite facies" in a greenstone belt in Sweden, where

28. 15 The latter is further sub - divided into gravelly and sandy braided fluvial facies.

29. The inner subfacies of extrusive facies of subaqueous volcanic rocks are good reservoirs.

30. 23 Permeability heterogeneity in plane is an important characteristic of fluvial facies formation.

31. 7 The main sedimentary system includes fluvial, delta, alluvial fan and lake facies.

32. The facies are sometimes described as 'bird-like' with a Beaked nose, brachycephaly, and micrognathia

33. The abandoned channel micro facies of fluvial reservoir blocks the fluid in the lateral.

34. Holes surface pore focus on upper and middle subfacies of effusive facies which locates edifice slope.

35. The region contains pelitic schists metamorphosed to lower to middle almandine–amphibolite facies.

36. The Urgonian facies completely surrounds the Parentis Basin and persists into the Albian.

37. 30 Introduced is a method for predicting sedimental sand body with fluvial facies.

38. Brecciation originates in numerous ways, resulting in highly complex classification systems and frequent misinterpretations of facies

39. To some extent, the facies evolution reflects the tectonic controls on the sedimentation of foreland basin.

40. 18 Highstand System Tract mainly develops depositional system of offshore - meare, fluvial facies and prograded delta.

41. Highstand System Tract mainly develops depositional system of offshore - meare, fluvial facies and prograded delta.

42. The basin facies area, however, is mainly with deep-water sediments characterized by radiolarian silicalite.

43. Amphibolite facies, one of the major divisions of the mineral-facies classification of metamorphic rocks, the rocks of which formed under conditions of moderate to high temperatures (500° C, or about 950° F, maximum) and pressures.

44. • Allergic facies: dark circles under eyes, folds below eyes, transverse crease over bridge of nose, adenoid facies caused by chronic mouth breathing, deep nasolabial folds, high arching of palate, enlargement of tonsils and adenoids

45. Rhyolite and Andesite are developed mainly in the effusive facies of Well Blocks DD14 and DD10

46. The stagnant marine phreatic zone of the Liassic facies types is indicated by late sediment consolidation.

47. 6 The abandoned channel micro facies of fluvial reservoir blocks the fluid in the lateral.

48. Granulite- and amphibolite-facies metamorphism was superimposed during the rapid uplift of high-pressure rocks.

49. Facies-analysis and biostratigraphic data indicate to an Upper Oxfordian age of the deeper stages of mound development.

50. Sedimentary facies indicate that the Bayan Mandahu redbeds were deposited in semiarid, alluvial to eolian environments.