Nghĩa của từ nummulitic facies bằng Tiếng Việt

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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.