1. The petitioned substance, Acidified sodium chlorite (ASC) solution, is a binary composition that consists of sodium chlorite solution and citric acid

2. Antigorite is present with chlorite in some rocks

3. Uents include Bastite, pyrite, mica (probably biotite), chlorite, and perhaps cliachite

4. Antigorite (massive serpentine), chlorite, kaolinite, Bementite, and brushite interfere

5. INTERFERENCES: Antigorite (massive serpentine), Chlorite, Kaolinite, Bementite, and Brushite interfere

6. Acidic aqueous chlorite teat dip providing shelf life, sanitizing capacity and tissue protection

7. Authigenic chlorite mineral appears quite abundantly and illite is less frequently

8. Chlorite is also a common metamorphic mineral, usually indicative of low-grade metamorphism.

9. Silicates (muscovite, albite, chlorite, labradorite, actinolite, and orthoclase) occur in high concentrations.

10. Patches are mainly epidote, quartz, hornblende, with minor albite, chlorite, apatite, and sphene.

11. The rocks commonly are altered to talc with carbonate or serpentine, chlorite, and magnetite.

12. These lamellar (flat, planar) minerals include micas, chlorite, talc, hornblende, graphite, and others.

13. Magnetite carries many inclusions such as apatite, amphiboles, chlorite, albite, carbonates, brucite and spinel exsolutions.

14. Generally oxidative Bleachings are carried out using sodium hypochlorite, sodium chlorite or sulfuric acid

15. Alteration minerals such as sericite and chlorite are also present in the veins and wall rocks.

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

17. Staurolite-formation in paragonite-rich micaschists is due to the reaction: chlorite + + paragonite + quartz = staurolite + albite + H2O.

18. When added to water, Chlorine dioxide forms chlorite ion, which is also a very reactive chemical

19. Indophenol blue color is produced in an alkaline borate medium using phenol and hypo-chlorite as reagents.

20. Later-stage vein minerals comprise chlorite, albite, and manganoan calcite which were deposited under less highly oxidizing conditions.

21. Sams Creek Metabasalt - Altered basaltic flows, some Amygdaloidal; green, schistose, containing hornblende, epidote, chlorite, and quartz

22. Amiant is actually whitish, but is often coloured green by chlorite or yellow by iron hydroxide (limonite)

23. Untreated and alkali-treated samples were pulped to various stages of delignification by the acid chlorite process.

24. Prase gets its light green color from Actinolite or Chlorite inclusions rather than the Fucshite inclusions of Green Aventurine.

25. The zoning is described as an exchange reaction with coexisting sheet silicates (mica or chlorite) and albite.

26. Fractures filled with quartz, calcite, ankerite, white mica, chlorite, pyrite, and native gold cross-cut the stock and its aureole.

27. Among the deposits, drill core samples of the North Anomaly are composed of magnetite, actinolite, chlorite, calcite, apatite, and other minerals.

28. Basaltic lavas are frequently spongy or pumiceous; the steam cavities become filled with secondary minerals such as calcite, chlorite, and zeolites

29. Occasionally trace amounts of copper-rich sulphides accompanied by platinum-group minerals occur only with the chlorite-clinopyroxene-spinel alteration assemblage.

30. Two types of alteration are developed in vicinity of quartz veins; i.e., sericite-quartz-pyrite and chlorite-epidote-pyrite-sericite alteration.

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

32. Naturally occurring form of hydrous magnesium silicate containing varying proportions of such associated minerals as alpha-quartz, calcite, chlorite, dolomite, magnesite, and phlogopite.

33. Coexisting minerals with beryl are quartz, plagioclase, K-feldspar, biotite, muscovite, margarite, chlorite, talc, amphibole, epidote, garnet, phenakite, calcite, fluorite (+accessory phases).

34. 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.

35. The Ag–, Co–Ni–sulpharsenide deposits of the Cobalt–Gowganda district are characterized by relatively uniform light-stable-isotope systematics, where δ18O in quartz spans 11.1–16.0‰; in K-feldspar, 10.1–12.3‰; in albite, 8.1–14.4‰; in actinolite, 6.0–7.6‰; in chlorite, 3.2–5.6‰; and δD in chlorite = −42 to −35‰.

36. Brucite may form as a standalone mineral, but it can also form as layers within minerals of the chlorite group and clay minerals such as …

37. Lodged within a fine-grained matrix of chlorite, white mica, quartz and albite are millimeter-sized clasts of quartz, plagioclase (albite or oligoclase) and epidote.

38. Acidified sodium chlorite solution: A potential prophylaxis to mitigate impact of multiple exposures to COVID-19 in frontline health-care providers Hosp Pract (1995)

39. Naturally occurring form of hydrous magnesium silicate containing varying proportions of such associated minerals as alpha-quartz, calcite, chlorite, dolomite, magnesite, and phlogopite

40. Sodium chlorite, like many oxidizing agents, should be protected from inadvertent contamination by organic materials to avoid the formation of an explosive mixture.

41. The garnets occur intergrown with secondary prehnite, pumpellyite, epidote and chlorite along biotite cleavage planes and formed through retrogradation of nearby plagioclase, almandine-rich garnet and hornblende.

42. Usually it coexists with hornblende or actinolite, magnesium clinochlore chlorite, talc, serpentine-antigorite minerals or metamorphic pyroxene.Magnesium-rich Cummingtonite can also coexist with anthophyllite.

43. Allothigenic clay minerals, particularly of the platy type (kaolinite, hy- dromica, chlorite, montmorillonite, vermiculite), are characterized by isometrical Fig.5. Allothigenic hydromica, Lower Devonian, Volga-Ural region

44. Stage 1 minerals include iron-rich barroisite, epidote, chlorite, paragonite, phengite, albite, quartz, ilmenite, magnetite, pyrite and occur only as inclusions in the core of eclogite garnets.

45. 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

46. 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.

47. FOREST COUNTY: Small grains of Andradite, usually with chlorite rims occur in outcrops of the McCaslin Quartzite at the Deer Lookout on Tower Hill in T.34N.

48. The first metamorphic event produced three calcite-free sub-greenschist facies assemblages that contain ubiquitous quartz+albite+titanite+chlorite+epidote along with pumpellyite or prehnite or actinolite.

49. A regional metamorphic process under conditions of the staurolite-almandine-subfacies ofWinkler’s andTurner andVerhoogen’s almandine-amphibolite facies transformed this assemblage to (2): cummingtonitic hornblende I+Mg-chlorite I (clinochlore)+talc.

50. 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.

51. 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

52. Indeed, epidote, chlorite, and quartz (related to the hydrothermal alteration) fill veins up to 10 mm wide, which crosscut the dolerite, developed contemporaneously to the Brecciation because they crosscut the breccia or are fragmented into the breccia

53. Amygdules or Amygdales form when the gas bubbles or vesicles in volcanic lava (or other extrusive igneous rocks) are infilled with a secondary mineral such as calcite, quartz, chlorite or one of the zeolites

54. The sediments from the Moresby Canyon, the Coral Sea Abyssal Plain, and the northeastern slope of the Queensland Plateau have received their terrigenous components, mainly quartz, feldspar, chlorite and muscovite-illite from mainland New Guinea.

55. Augite is an important rock-forming mineral, and large crystals are fairly common. It is the most widespread member of the pyroxene group, and it frequently alter s to many other minerals, including Hornblende, Chlorite, and Epidote

56. In rock samples of a Middle Devonian spilitized basaltic sill near Langelsheim (Northwestern Harz Mountains) the following mineral assemblage: pumpellyite + prehnite + epidote + actinolite grown in a groundmass of albite, chlorite, calcite and quartz has been studied by use of a microprobe.

57. The piezoelectric mineral composition (3) is constituted essentially by 10-30 % of albite, preferably 15 %, 20-40 % of tourmaline, preferably 30 %, 10-50 % of quartz, preferably 30 %, 10-20 % of chlorite, preferably 13 % and 10-20 % of illite, preferably 12 %.

58. Amygdules or Amygdales form when the gas bubbles or vesicles in volcanic lava (or other extrusive igneous rocks) are infilled with a secondary mineral such as calcite, quartz, chlorite or one of the zeolites.Amygdules usually form after the rock has been emplaced, and are often associated with low-temperature alteration

59. 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.

60. The mineral assemblages are dominated by muscovite (25–45%), chlorite (15–25%), quartz (18–30%) and albite (2–6%) while hematite, dolomite, pyrite, apatite, ore, zircon, rutile and amorphous carbon are accessory, but in some rocks hematite (11%), dolomite (42%) and talc (40%) are also dominant.

61. Inorganic Anions refer to the combination of: Common Anions: chloride, fluoride, bromide, nitrate, nitrite, sulfate, and phosphate; Inorganic disinfection byproducts (DBPs): chlorate, chlorite, and bromate; Other Anions, such as perchlorate and chromate.; Chloride and sulfate are also matrix Anions due to their high concentration in certain drinking water samples.

62. Two samples contain pyrope-rich gamets but coexisting pyroxenes are extremely magnesian and temperatures of equilibration of both primary omphacite-pyrope and secondary omphacite-almandine/pyrope-chlorite are only slightly higher (500–650° at 10 kbar) than those for almandine jadeite eclogites and estimates overlap with those of some examples of the latter type.

63. Two significant alteration assemblages are amphibole (actinolite) + epidote + chlorite + quartz ± albite ± K-feldspar ± calcite adjacent to Cu-rich veins in the Deep Copper Zone of Strathcona mine and the nearby Barnet property, and amphibole (actinolite to ferro-actinolite) + epidote + titanite + pentlandite + pyrite ±quartz ± magnetite in the Fraser mine Epidote Zone.

64. The clay-sized (< 2 μm) fraction of the silty and arenaceous lutites constituting CESAR cores 14 and 103 (Alpha Ridge, central Arctic Ocean) is composed predominantly of mica (40–60%), with subequal percentages (10–20%) of kaolinite and chlorite and lesser amounts (< 5%) of smectite, quartz, plagioclase, and potassium feldspar.

65. 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.