1. Green schist, garnet schist, mica- garnet schist

2. Garnetiferous schist, quartz-mica schist, Calcareous schist, schistose marble, hornblende bearing quartz mica schist and micaceous marble

3. It is a tectonically composed pile of marbles alternating with glaucophane schists, actinolite schists and chlorite schists.

4. Abraham Schist in the Lincoln Gap area are lithically similar to the Albitic and chioritoid bearing schists of the allochthonous Hoosac Formation and the Greylock slice in western Massachusetts

5. Schist vs Amphibolite Characteristics

6. Schist Villages’ network is implementing a set of Schist Walking Trails.

7. Schist vs Amphibolite characteristics assist …

8. Look at all this schist

9. The Albitic Hazens Notch schist and Mt

10. While garnetiferous schist, Calcareous schist and quartzite, being relatively strong and intact rocks, are characterized in class A, B and C.

11. The Marampa Schists are renamed the Marampa Formation.

12. The foot wall consists of a Bowldery or brecciated schist

13. The bedrocks consist of garnet mica schists with occasional staurolite.

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

15. Below the Génis sericite schist follows the Puy-de-Cornut arkose.

16. Regarding the soil, the parent material is schist, which usually means poor soil

17. Regarding the soil, the parent material is schist, which usually means poor soil.

18. Building and constructions materials comprised from schist, silica quartz or glass granules

19. Two grades of metamorphism, both subfacies of the greenschist facies of regional metamorphism, were mapped on the Araya Peninsula: 1. the quartzalbite-epidote-almandine subfacies, consisting mainly of a sequence of garnet and kyanite quartz-mica schists, interlayered with quartzites; and 2. the quartzalbite-muscovite-chlorite subfacies, which consists of chloritic phyllites, quartzmica schists and phyllites, metaconglomerates, calcareous quartz-mica schists, limestones and marbles, and calcareous epidote schists of volcanic origin.

20. This base is probably Cambrian and comprises a seam of porphyroid granite and schist.

21. The shear zones developed in granite-gneisses, gneiss-phyllonites and mica-schists.

22. Description: Andalusite is found in phyllites, schists and gneisses and associated quartz veins

23. A special feature is the Posidonia schist (Lias epsilon), which is 10 m thick.

24. Some of the trace elements were also mobile: Compared to serpentinite, Li and Be were enriched in all the blackwall rocks, and Sn and Cs in the actinolite, chlorite, and biotite schists; Sr was concentrated in the dolomite-bearing talc schists, and Zn, Rb, and Ba predominantly in the biotite schists.

25. Boundary layers between diopsidic tale-silicate rocks and associated pelitic schists are described.

26. It covers an autochthonous block composed of migmatites and mica-schists and their cover.

27. This base is probably Cambrian and comprises a seam of porphyroid granite and schist

28. The main rock types include granulitite, mica schist, epidote-plagioclase amphibolite,[http://Sentencedict.com] itabirite and marble.

29. The rock consists of phyllites and schists, and is highly susceptible to weathering and erosion.

30. The Cretan stone that was used at the time included steatite, stalagmite, alabaster, schist, and serpentine.

31. Weneg's name appears in black ink inscriptions on alabaster fragments and in inscriptions on schist-vessels.

32. Recent reworked deposits of alluvium cover surface deposits of silty clay that overlay clay schist bedrock.

33. The survey included streams on granite (13), schist (16), basalt (6), limestone (7) and sandstone (5).

34. They intersect Precambrian country rocks composed of potassium feldspar-biotite-granitic-mobilisates and chloritised biotite mica schists.

35. In our area lepontine garnet-staurolite-kyanite-schists abut directly against the Insubric line and the Seealpen.

36. Biotite is also common in metamorphic rocks where it is a frequent component of schists, gneisses and phyllites

37. The dyke-quartz-masses of the Bavarian “Pfahl” are embedded in schists striking NW-SE.

38. This paper is concerned with a laboratory study carried out on samples of weathered Athenian Schists.

39. In adjacent, partly almandine-bearing biotite-quartz-plagioclase schists, plagioclase ranges from sodic andesine to bytownite.

40. 13 The middle Proterozoic crystalline schist series in the Panzhihua - Xichang region has undergone progressive regional metamorphism.

41. Occurrences of chrome, asbestos, talc and nickel are associated with ultramafic rocks within greenstone and related schist belts.

42. Schellkopf, Brenk, Brohltal, Ahrweiler District, Rhineland-Palatinate, Germany : Active phonolite quarry (selbergite, selbergite tuffs, Devonian schists) on Schellkopf mountain

43. General characteristics for distinguishing apogranite greisens affected by regional metamorphism from metapelitic mica schists are given.

44. Associated non-calcareous mica schists, commonly with almandine and kyanite, carry more sodic plagioclase which is unzoned.

45. The sulphides have been deformed in the retrograde schist zones and the ore therefore predates this event.

46. There are a number of Na-Amphiboles, all typcally found in high pressure (especially blue schist facies) metamorphic rocks

47. Soils formed from the decomposition of granites and schists are acid, sandy, filtering and poor in clay.

48. Calcite is an accessory mineral in both the grey and green schists at <5% of the rock.

49. This rock unit consists Chieflyof Silurian shale and sandstone that have been metamorphosed to high-grade schist and migmatite

50. Beryl is a minor constituent of many granitic rocks and associated pegmatite dikes, in gneisses, and in mica schists

51. 16.1 and 16.2A).This lithological unit exhibits important variations in mineralogical proportions ranging from garnet-biotite schist to Cummingtonite–plagioclase amphibolite.

52. Precambrian amphibolites and quartz-mica schists in the Saidapuram-Podalakuru area fall within the almandine-amphibolite facies of regional metamorphism.

53. The Allochtons are mainly in the area of lustrous schists and ophiolites corresponding to the eastern relief (Cap Corse and Castagniccia)".

54. Boniest •assist, cist, coexist, consist, cyst, desist, enlist, exist, fist, gist, grist, hist, insist, list, Liszt, mist, persist, resist, schist, subsist, tryst

55. Description: Anatase is a relatively rare mineral found in veins and cavities in schists, gneisses, granites, syenites and other related igneous rocks

56. (It’s the opposite of human aging: Cragginess is a sign of relative youth, and smoothness comes only with time.) And the words! Schist

57. It is associated with mica schist which increases alkali content in ultimate product and so it has not been exploited economically so far.

58. Almandine is the most common of the garnets and is usually the garnet found in garnet schists (a type of metamorphic rock composed mostly of mica)

59. Cale-silicate mica schists of higher-medium grade carry mutually stable calcic scapolite, andesine and zoisite, associated with calcite, quartz, local epidote, biotite, muscovite, and garnet.

60. 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.

61. It is a common alteration product of periclase in marble; a low-temperature hydrothermal vein mineral in metamorphosed limestones and chlorite schists; and formed during serpentinization of dunites.

62. 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.

63. Cherts Sentence Examples Lower Cretaceous limestones and schists, with radiolarian Cherts, are extensively developed; and in many parts of the island Upper Creta 1 See L.

64. The village is dominated by the "red lands", which are rubble of the industrial calcination of Alumiferous schists required to produce alum (XVIth-XIXth centuries)

65. Andradite is found in skarns from contact metamorphosed impure limestones or calcic igneous rocks; in chlorite schists and serpentinites; in alkalic igneous rocks, then typically titaniferous.

66. Within the belt , the mid-late Proterozoic (epimetamorphic) green- schists were ovethrust from south to north onto the late Paleozoic granitic batholith at a low angle.

67. The series consists of silty sericite schists, ordinary and conglomeratic greywackes, arkosic sandstones, thinly banded slates of varvitic type, conglomerates and volcanites, i. e. spilitic porphyrites and amygdaloids, tuffs and quartz keratophyres.

68. Widespread reverse zoning of this plagioclase is attributed to slow, short-range (a few centimeters) diffusion of anorthite-building substance from the adjacent Ca-richer rock into the schist.

69. Andradite occurs “in skarns from contact metamorphosed impure limestones or calcic igneous rocks, in chlorite schists and serpentinites, [and] in alkalic igneous rocks, [where there are] then typically titaniferous

70. Alum (aluminium potassium sulfate) was produced by calcination of Alumiferous schist, aka ampelite (from Greek, ampelos, "grapevine"), and used locally to fertilize the vineyard of the valley of the Meuse

71. Amphibolite facies metamorphism at Jack Hills is denoted by the presence of grunerite in BIF and the association of calcic plagioclase and hornblende in mafic schist and Amphibolite (Wilde and Pidgeon, 1990)

72. Almandine, the most common of the garnets, is deep red to brownish-red and is found in metamorphic rocks, such as schists and gneisses, in association with micas, quartz, and feldspars

73. (adjective) Thus, we find them more frequently, folded, tilted and Cleaved; the muds have become shales, slates, phyllites or schists, the grey and red sands and conglomerates have become quartzites and greywackes, while …

74. The post-Cambrian marine sedimentation is made up of alternate layers of limestone, dolomites, schists and clays, with the successive series of Pliocene sedimentations represented by basal conglomerates, marls, clays and finally loose sandstones and sand

75. Amphibole - Cummingtonite w- chlorite in schist Magnesium iron silicate 3800 foot level Homestake Mine Lawrence COunty South Dakota 2071.jpg 568 × 470; 93 KB Auriferous greenschist 2, Homestake Mine.jpg 2,937 × 1,461; 5.07 MB

76. The post-Cambrian marine sedimentation is made up of alternate layers of limestone, dolomites, schists and clays, with the successive series of Pliocene sedimentations represented by basal conglomerates, marls, clays and finally loose sandstones and sand.

77. Flower Jade, Nephrite Jade, Black Nephrite Jade Cabochons: Cabochons Gallery 69 : Chrysocolla and Malachite, Parrot Wing Chrysocolla Cabochons: Cabochons Gallery 70 : Garnet in Schist Cabochons: Cabochons Gallery 71 : Tiffany Stone (Bertrandite) Cabochons: Cabochons Gallery 72 : Marra Mamba Tiger Eye Cabochons

78. ‘The prominent basement rocks of the Brumado area are Precambrian in age and consist dominantly of gneisses, schists, and Amphibolite.’ ‘A uniform, regionally concordant layer of Amphibolite with occasional ultramafic pods, termed the Sta Amphibolite, overlies the Sta Series.’

79. Geologically, the west of Corsica is Hercynian, dominated by granites, granulites and porphyries, which produce a landscape of high rocky peaks, and the northeast is Alpine, with lustrous schists and various sedimentary terrains, lower altitudes and less towering reliefs.

80. Geologically, the west of Corsica is Hercynian, dominated by granites, granulites and porphyries, which produce a landscape of high rocky peaks, and the north-east is Alpine, with lustrous schists and various sedimentary terrains, lower altitudes and less towering reliefs.