Lec 7 - Geothermometry, Geobarometry, And Istope Studies Flashcards

1
Q

What are your persitent minerals

A

Pyrite and gold

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2
Q

At surface conditions: oxides suffers ______, and sulfides suffers __________

A

Oxides suffers least and sulfides suffers most

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3
Q
  • greek word means “born beside”
  • used to describe any assemblage of ore minerals, with or without gangue, formed at the same time and normally in equilibrium.
A

Paragenesis

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4
Q

A collection or gathering of minerals or rock

A

Assemblage

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5
Q

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

A

Associated

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6
Q

Minerals that yield information as to the temperature of their formation

A

Geothermometers

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7
Q

The measurement of lavas, fumaroles, and hot springs

A

Direct Measurement

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8
Q

Indicate the maximum crystallization temperatures

A

Melting points

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9
Q

Hot spring measurements

A

Opal, gypsum, stibniteu

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10
Q

Some minerals lose volatile content at certain temperatures

A

Dissociation

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11
Q

Transformation of some minerals’ crystal sytem to naother is temp dependent

A

Inversion points

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12
Q

Minerals that form solid solutions unmix at specific temps to yield distinguishable intergrowths

A

Exsolution

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13
Q

Similar to inversion and exsolution but applies more specifically to native minerals

A

Recrsytallization

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14
Q

Crystals trap gases or liquids which they crystallizes

A

Fluid inclusion

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15
Q

Fluid inclusions in cavities of crystals indicate the ______________ of formation of the crystals by the amount of contraction of the liquid, assuming the liquid originally filled the cavity

A

Approximate Temperature

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16
Q

Heating the sample until an heterogenous fluid inclusion homogenizes

A

Minimum Temperatures of Formation

17
Q

By freezing-point depression method. This temp is then used to read off the solution composition from a graph or calculated from equations

A

Total NaCl-equivalent salinity of the fluid

18
Q

The minimum melting point

A

Eutectic point

19
Q

Inclusion is opened up and direct tests are made on the liquid by optical-physical properties

A

Composition of Ore-Bearing fluid

20
Q

Inclusions formed in growing crystals with no leakage

A

Primary

21
Q

Inclusions that formed With fractures and sealed again,records comdition of later hydrothermal stage. Formed after primary crystallization

A

Secondary

22
Q

Looks like secondary, but the host crystal was fractured as the crystal was growing

A

Pseudosecondary

23
Q

It is important to remember always that the fluid inclusions in a mineral provide information only on the fluids present at the time of sealing of the inclusion, whether that be during the growth of the host crystal or during rehealing of a later fracture

A

Edwin Roedder, 1977

24
Q

The estimation of pressure conditions at which a geologic material formed.

A

Geobarometry

25
Q

Determine the source and composition of ore-bearing fluids/components, age of mineral deposit, dteermine temperature and other conditions of deposition, and to establish the degrees of bacteriological involvement in certain ore-forming processes

A

Isotope studies

26
Q

Does not decay into other elements

A

Stable isotope

27
Q

Able to classify source of water in hydrated alteration minerals

A

Oxygen (18) and Hydrogen (D) isotopes

28
Q

It pinpoints the source of sulphur,

A

Sulphur (35 and 34) isotopes

29
Q

(Decay) into daughter istopes at known rates

A

Radioisotopes

30
Q

Amount of time needed for one-half of a radioactive parent to decay into daughter isotopes

A

Half-life

31
Q

Establish the time of origin of a rock by a momount of common lead it contains

A

Uranium-Thorium-Lead (U-Th-Pb)

32
Q

The single set of lead isotope ratios throughout the earth mass during the formation of earth

A

Primitive lead