sulfides 9-12 SET 3 Flashcards

1
Q

Realgar formula

A

As4S4

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2
Q

Realgar crystal form

A
  • monoclinic, uncommon crystals
  • coarse to fine grained earthy encrustations
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3
Q

Realgar cleavage

A

pinacoidal good

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4
Q

Realgar hardness

A

1.5 to 2 sectile

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5
Q

Realga specific gravity

A

3.48

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6
Q

Realgar color

A

resinous, transparent to translucent. red to orange and red to orange streak

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7
Q

Realgar occurrence

A
  • in hydrothermal veins with orpiment
  • assoc with lead and silver minerals and well as stibnite
  • as volcanic sublimation product
  • deposit from hot springs
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8
Q

Realgar remarks

A

red color, orange red streak, resinous luster and invariable assoc with orpiment

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9
Q

orpiment formula

A

As2S3

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10
Q

orpiment crystal form

A
  • monoclinic, rare crystals
  • usually foliated, columnar, or fibrous masses
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11
Q

orpiment cleavage

A

pinacoidal perfect 010. flexible cleavage laminae, not elastic

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12
Q

orpiment hardness

A

1.5 to 2 sectile

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13
Q

orpiment specific gravity

A

3.49

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14
Q

orpiment color

A

resinous translucent. lemon yellow, pale yellow streak

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15
Q

orpiment occurrence

A
  • rare mineral
  • assoc with realgar, formed same conditions
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16
Q

orpiment remarks

A
  • yellow color
  • foliated structure
  • excellent cleavage
17
Q

how to differentiate orpiment and sulfur?

A

orpiment has perfect pinacoidal cleavage, sulfur has none, only conchoidal fracture.

also orpiment is sectile, sulfur is brittle

18
Q

stibnite formula

A

Sb2S3

19
Q

stibnite crystal form

A
  • orthorhombic common crystals
  • slender prismatic, with vertical striations in prism zone, the prisms appear bending or twisted bc of translation gliding
  • often in radiating crystal groups or bladed forms with prominent cleavage
  • massive coarse to fine granular
20
Q

stibnite cleavage

A

perfect pinacoidal 010, paralle striations 100

21
Q

stibnite hardness

A

2

22
Q

stibnite specific gravity

A

4.52 to 4.62

23
Q

stibnite color

A

metallic opaque. (very color on cleavage).
lead gray to black, same with streak

24
Q

stibnite occurrence

A
  • in low temp hydrothermal veins or replacement deposits
  • in hot spring deposits
  • in assoc with other antimony minerals that formed as a product of its decomposition, with galena cinnabar, sphalerite, barite realgar orpiment and gold
25
Q

stibnite remarks

A

bladed habit, perfect one direction cleavage, lead gray color, soft black streak

26
Q

stibnite remarks

A

bladed habit, perfect one direction cleavage, lead gray color, soft black streak

27
Q

how to distinguish stibnite from galena

A

stibnite has a perfect pinacoidal cleavage, galena has perfect cubic.

it also is orthorhombic while galena is isometric

stibite also has lower specific gravity

28
Q

how to distinguish stibnite from galena

A

stibnite has a perfect pinacoidal cleavage, galena has perfect cubic.

it also is orthorhombic while galena is isometric

stibite also has lower specific gravity

29
Q

pyrite crystal form

A
  • isometric, striated cube faces, pyritohedron, octahedron
  • massive, granular, reniform, globular
30
Q

pyrite cleavage

A

none. conchoidal fracture, brittle

31
Q

pyrite hardness

A

6 to 6.5

32
Q

pyrite specific gravity

A

5.02

33
Q

pyrite color

A

pale brass yellow, darker because of tarnish. streak greenish to brownish black

34
Q

pyrite occurrence

A
  • formed in high and low temperatures
  • as magmatic segregation, accessory to igneous rocks, contact metamorphism and hydrothermal veins
  • common in shales and limestone
  • in vein deposits assoc with many mineral esp chalco, sphalerite and galena
35
Q

how to tell pyrite from gold

A

pyrite is paler in color, and also harder and brittle

36
Q

how to tell pyrite from marcasite

A

marcasite is even paler in color, marcasite is also orthorhombic while pyrite is isometric

37
Q

what mineral is easily altered from pyrite and what often results because of this?

A

limonite, often pseudomorphism results

38
Q

usually there is a capping of limonite in pyrite veins, what’s this called

A

gossan