問題一覧
1
Occur in native state, uncombined form
Native Elements
2
Cu,Au,Ag,S,Diamond
Native Elements
3
Pure masses if single metal/ element
Native Elements
4
S2- bonded to metal cation
Sulfides
5
Economically important as metal ores
Sulfides
6
pyrite, galena
Sulfides
7
(SO4)2- bonded to metal action
Sulfates
8
Many forms by precipitation out of highly saline water at and/or near the Earths surface
Sulfates
9
Gypsum, Barite
Sulfates
10
Metal cations combined with oxygen
Oxides
11
Can be simple or multiple
Oxides
12
Strong Ionic bonding,hard, dense, and refractory
Oxides
13
Form many of the valuable ores
Oxides
14
Also carry the best record of changes in the earths magnetic field
Oxides
15
Hematite, Magnetite, Chromite, Pyrolusite, manganite
Oxides
16
Metals attached with (OH)-
Hydroxides
17
Tend to be less dense than oxides, and not as hard
Hydroxides
18
Form at low temp, and predominantly in weathering products (alteration in hydrothermal veins)
Hydroxides
19
Manganite (MnO(OH)), diaspore, Geothite
Hydroxides
20
Contains halogen ions like Cl- or F-
Halides
21
Salts that form when salt water evaporates
Halides
22
Low hardness, poor thermal and electric conductors when solid, good electric conductors when molten
Halides
23
Halite(NaCl), Flourite (CaF2), Sylvite KCl
Halides
24
Silica Tetrahedon, as fundamental component
Silicates
25
______ minerals make up over 90% of crust
Silicates
26
Contain (CO3)2-
Carbonates
27
Commonly deposited in marine settings when the shells of dead planktonic life settle and accumulate on the sea floor
Carbonates
28
Calcite, Azurite, Malachite, dolomite
Carbonates
29
Similar structure with silicates but instead of Si, its P, As (arsenates), or Va (Vanadates)
Phosphates
30
turquoise
Phosphates
31
Single, isolated tetrahedron No cleavage Composition: (Mg, Fe)2SiO4
Neosilicates/ Olivine Group
32
not stable in the presence of free quartz and will form a pyroxene called enstatite
Forsterite
33
•Structure possessing parallel silica letrahedron chains whuch can be double or single • Single/Pyroxene Group • Double/ Amphibole Group
Inosilicates
34
Cleavage: 2 at 90 deg Orthopyroxene Clinopyroxene
Single/ pyroxene Group
35
Common in peridotites, gabbros, norutes and basalts Commonly associated by olivine, pagioclase, Ca-rich clinopyroxene
Enstatite
36
Monoclinic Augite
Clinopyroxene
37
Most common pyroxene mineral
Augite
38
• Hornblende • cleavage: 2 at 60 deg and 120 deg • in the presence of water/fluids, pyroxenes are often converted to amphibole
Double/ Amphibole group
39
Ca-rich amphibole mineral, common in diorites, commonly occurs with pagioclase
Hornblende
40
Sheets of silicate tetrahedron cleavage: 1 plane Biotite Muscovite
Phyilosilicates/ Mica Group
41
Dark colored mica common in granite, diorite, gabbros, and peridotites
Biotite
42
Mg-rich if in unltramafics and Fe-rich if in granites
Biotite
43
In metamorphic rocks, it occurs with chlorite and muscovite
Biotite
44
Light colored mica common in granites
Muscovite
45
3D framework if silicate tetrahedron Feldspar Silica Group
Tectosilicates
46
•Potassium Feldspar/ Orthoclase/ Alkali Feldspar • Calcium Feldspar/ Pagioclase • Sodium Feldspar / Albite
Feldspars
47
Most abundunt silicate mineral in the crust
Calcium Feldspar/ Pagioclase
48
Quartz, Opal , Chalcedony
Silica Group
49
Tridymite or cristobalite in high temp
Quartz
50
Rose,admethyst and smoky ____ are low temp varieties
Quartz
51
common in granite, diorite and chert
Quartz
52
common in gangue mineral in hydrothermal ore deposit
Quartz
53
Quartz with water
Opal
54
along with chalcedony and agate, they occur in hydrothermally altered rocks
Opal
55
Fibrous Variety
Chalcedony