Day 2 Pretest Flashcards

1
Q

Point Counting Method

A

A technique in petrography that involves traversing a thin section in a grid and counting minerals at each grid point to determine modal composition.

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2
Q

Mode of a Rock

A

The proportion of minerals in a rock, expressed as a percentage of volume or weight.

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3
Q

Becke Line Movement

A

A bright line seen around a mineral grain in a liquid of different refractive index, used to determine whether the mineral has a higher or lower RI.

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4
Q

Idiochromatic Minerals

A

Minerals that exhibit color due to their inherent composition, such as Azurite (blue) and Cinnabar (red).

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5
Q

Allochromatic Minerals

A

Minerals that owe their color to trace impurities or structural defects, such as Amethyst (purple quartz with iron).

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6
Q

Cinnabar

A

The primary ore of mercury, composed of mercury sulfide (HgS), and known for its deep red color.

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7
Q

Metamorphic Facies

A

A set of metamorphic mineral assemblages that develop under specific pressure-temperature conditions, such as greenschist and granulite facies.

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8
Q

Troctolite

A

A coarse-grained, igneous rock composed primarily of olivine and plagioclase feldspar, belonging to the gabbro family.

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9
Q

Pleochroism

A

The optical property where a mineral displays different colors when viewed under polarized light from different angles.

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10
Q

Dichroism vs. Trichroism

A

Dichroism occurs in uniaxial minerals (two colors), while trichroism occurs in biaxial minerals (three colors).

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11
Q

TAS Diagram

A

A classification diagram for volcanic rocks based on total alkali (Na₂O + K₂O) and silica (SiO₂) content.

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12
Q

Undulose Extinction

A

A wavy extinction pattern observed in quartz and other minerals under a microscope, caused by strain deformation.

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13
Q

Desert Rose

A

A flower-like gypsum crystal formation that occurs in arid environments due to seasonal water fluctuations.

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14
Q

Solidus vs. Liquidus

A

Solidus is the temperature below which a substance is entirely solid, while liquidus is the temperature above which it is entirely liquid.

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15
Q

Tie Line in Phase Diagrams

A

A horizontal line connecting two coexisting phases in equilibrium within a two-phase region of a phase diagram.

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16
Q

Melatope

A

The narrowest part of an isogyre in an interference figure, representing the point where an optic axis emerges.

17
Q

Isogyre vs. Isochrome

A

Isogyre refers to dark cross patterns in an interference figure, while isochrome refers to colored concentric rings.

18
Q

Adularia

A

A potassium feldspar that forms in low-temperature hydrothermal veins and resembles microcline but lacks tartan twinning.

19
Q

Peridotite

A

A coarse-grained ultramafic rock composed mostly of olivine, with varying amounts of pyroxene and hornblende.

20
Q

Botryoidal Texture

A

A mineral habit resembling a cluster of grapes, commonly seen in hematite and malachite.

21
Q

Geode

A

A hollow rock formation lined with mineral crystals, typically formed in volcanic or sedimentary rocks.

22
Q

Monzonite

A

An intrusive igneous rock containing nearly equal amounts of potassium feldspar and plagioclase feldspar.

23
Q

Norite

A

A type of gabbro rich in orthopyroxene, commonly associated with layered mafic intrusions.

24
Q

Eutectic Point

A

The lowest temperature at which a mixture of components can melt simultaneously, forming a single liquid phase.

25
Q

Peritectic Reaction

A

A reaction where a solid and a liquid combine to form a new solid at a specific temperature.

26
Q

Miscibility Gap

A

A region in a phase diagram where two immiscible phases coexist instead of forming a homogeneous mixture.

27
Q

Plagioclase Feldspar

A

A solid solution series between albite (NaAlSi₃O₈) and anorthite (CaAl₂Si₂O₈) found in igneous rocks.

28
Q

Metamorphic Rock Progression

A

Foliated metamorphic rocks progress from slate to phyllite, schist, gneiss, and granulite with increasing metamorphism.

29
Q

Udden-Wentworth Scale

A

A grain size classification system for sediments, ranging from clay to boulders.

30
Q

Miller Indices

A

A system used to describe the orientation of crystal planes in a crystal lattice.

31
Q

Interference Colors

A

Colors seen in thin sections under cross-polarized light due to variations in birefringence.

32
Q

Extinction Types

A

Parallel extinction occurs when a mineral goes dark along cleavage planes, while inclined extinction occurs at an angle.

33
Q

Crystal Forms

A

General forms are defined by Miller Indices {hkl}, while special forms are unique to specific crystal classes.

34
Q

Twin Laws

A

Common twin laws include Albite twinning in plagioclase, Carlsbad twinning in orthoclase, and Japan Law in quartz.

35
Q

Beryl Varieties

A

Beryl occurs in different colors: Emerald (green), Aquamarine (blue), Heliodor (yellow), and Morganite (pink).

36
Q

Radioactive Minerals

A

Common uranium-bearing minerals include Autunite, Torbernite, and Uraninite.

37
Q

Motif & Unit Cell

A

A motif is a repeating atomic arrangement, while a unit cell is the smallest repeating structure of a lattice.

38
Q

Folk’s Classification of Carbonates

A

A classification for limestones based on allochems (grains) and matrix/cement (micrite, sparite).

39
Q

Index Minerals of Metamorphism

A

Chlorite (low grade), Biotite, Garnet, Staurolite, and Sillimanite (high grade) indicate metamorphic conditions.