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

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

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
stibnite remarks
bladed habit, perfect one direction cleavage, lead gray color, soft black streak
26
stibnite remarks
bladed habit, perfect one direction cleavage, lead gray color, soft black streak
27
how to distinguish stibnite from galena
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
how to distinguish stibnite from galena
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
pyrite crystal form
- isometric, striated cube faces, pyritohedron, octahedron - massive, granular, reniform, globular
30
pyrite cleavage
none. conchoidal fracture, brittle
31
pyrite hardness
6 to 6.5
32
pyrite specific gravity
5.02
33
pyrite color
pale brass yellow, darker because of tarnish. streak greenish to brownish black
34
pyrite occurrence
- 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
how to tell pyrite from gold
pyrite is paler in color, and also harder and brittle
36
how to tell pyrite from marcasite
marcasite is even paler in color, marcasite is also orthorhombic while pyrite is isometric
37
what mineral is easily altered from pyrite and what often results because of this?
limonite, often pseudomorphism results
38
usually there is a capping of limonite in pyrite veins, what's this called
gossan