Geothermometry, Geobarometry & Isotope Studies Flashcards

1
Q

Sequence of deposition of minerals

A

Paragenesis

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2
Q

Collection pr gathering of minerals or rock

A

Assemblage

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3
Q

Having a connection or resemblance with other mineral in certain temperature and pressure regime

A

Associated

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4
Q

The spatial distribution of paragenesis

A

Zoning

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5
Q

The spatial distribution of paragenesis

A

Zoning

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6
Q

Born beside

A

Paragenesis

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7
Q

Measurement of lavas, fumaroles, hot springs

A

Direct Measurement

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8
Q

Indicate the maximum crystallization temperature

A

Melting Point

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9
Q

Some minerals lose their volatile content at certain temperature

A

Dissociation

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10
Q

Transformation of some minerals crystal system to another is temperature dependent

A

Inversion Point

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11
Q

Minerals that form solid solutions unmix at specidic temperatures to yield distinguishable intergrowths

A

Exsolution

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12
Q

Melting Point of Albite

A

1104C

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13
Q

Melting Point of Stibnite

A

546C

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14
Q

Melting Point of Bismuth

A

271C

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15
Q

Exsolution of

Chalcopyrite - Bornite

A

475C

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16
Q

Exsolution of

Cubanite - Chalcopyrite

17
Q

Exsolution of

Bornite - Chalcopyrite

18
Q

similar to inversion and exosoution but applies more specifically to native metals

A

Recystallization

19
Q

Recrystallization temp of

Cu
Ag

20
Q

Quartz lose color at

21
Q

Fluorite lose color at

22
Q

indicate the approximate temp of formation of the crystals by the amount of contraction of the liquid, assuming that the liquid originally filled the cavity

A

Fluid Inclusion

23
Q

heating the sample until heterogeneous fluid inclusion homogenizes

A

Filling Temperature (Minimum Temperature of Formation)

24
Q

by the freezing point depression method

A

Total NaCL-equivalent salinity of the fluid

25
The minimum melting point
Eutectic Point
26
inclusion is opened up and direct tests are made on the liquid by optical properties
Composition of the ore-blearing fluid
27
inclusions formed in growing crystals, no leakage
Primary
28
with fracture & sealed again, records conditions of later hydrothermal stage
Secondary
29
looks like secondary, but the host crystal was fractured as the crystal was growing
Pseudosecondary
30
commonly based on mineral assemblage and composition information
Geobarometry
31
estimation of pressure condition at which a geologic material formed
Geobarometry
32
an element that has a nuclei that does not change spontaneously
Stable isotope
33
decays into daughter isotopes at known rates
Radioisotopes
34
amount of time needed for one half of radioactive parent to decay
Half-life
35
is any Pb from a rock or mineral that contains a large amount of Pb and a small amount of the radioactive progenitors of Pb
Common Lead