01 - Rock Classification Flashcards

1
Q

Definition

Rock

A

naturally occurring aggregates of one (monomineralic) or more minerals (polymineralic).

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2
Q

Three major rock groups

A

Igneous rocks -> magmatites

Metamorphic rocks -> metamorphites

Sedimentary rocks -> sediments

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3
Q

Three main processes of rock cycle

A
  1. Erosion & sedimentation
  2. Melting & recrystallization
  3. Sink & recrystallization
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4
Q

Igneous rocks:

three types by occurence and position in crust

A

plutonic

volcanic

subvolcanic

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5
Q

Igneous rocks:

classification according to chemical / mineralogical composition

distingluishes .. (4)

A
  • felsic or silicic rocks (granite, rhyolite) -> acid
  • intermediate rocks (granodiorite, diorite, dacite, andesite)
  • mafic rocks (basalt, gabbro) -> basic
  • ultramafic rocks (peridotite, dunite)
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6
Q

Igneous rocks:
Streckeisen in Exercise 1
Mafic & Ultramafic clasification -> Bilder angucken
TAS

A

Streckeisen in Exercise 1
Mafic & Ultramafic clasification -> Bilder angucken
TAS

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7
Q

Metamorphic rocks:

classification … (4)

A
  • in low, medium, high grade
  • in metamorphic facies zones (mineral paragenesis)
  • after textures (slate, schist, gneiss, fels)
  • after origin (contact-, regional-, subduction-, shock-)
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8
Q

classification in low, medium, high grade:

Sort with increasing metamorphic grade:

  • schist
  • gneiss
  • slate
  • blueschist
  • phyllite
  • migmatite
A

Low grade:

  1. slate
  2. phyllite

Intermediate grade:

  1. blueschist
  2. schist

High grade:

  1. gneiss
  2. migmatite
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9
Q

in metamorphic facies zones:

name the 3 major types of metamorphic series

A
  1. High P/T Series
  2. Medium P/T Series
  3. Low P/T Series
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10
Q

in metamorphic facies zones:

  1. High P/T Series - facies?
A

Zeolite

  • > Blueschist
  • > Eclogite

(high increasing P and low increasing T)

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11
Q

in metamorphic facies zones:

  1. Medium P/T Series - facies?
A

Zeolite

  • > Greenschist
  • > Amphibolite
  • > Granulite

(increasing P and increasing T)

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12
Q

in metamorphic facies zones:

  1. Low P/T Series - facies?
A

Zeolite

  • > Hornfels (Ab-Ep -> Hornblende -> Pyroxene)
  • > Sanidinite or Granulite

( low increasing pressure and high ingreasing T

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13
Q

Sedimentary rocks:

name the 3 major rock classes

A
  1. clastic
  2. chemical
  3. organic
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14
Q

Sedimentary rocks - clastic:

formation processes

A
  • erosion, reworking, transportation
  • deposition & sedimentation
  • compaction and diagenetic processes
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15
Q

Sedimentary rocks - clastic:

what does the physical properties strongly depend on?

(was red marked in lecture)

A
  1. Textural properties:
    - particel dimensions
    - size
    - shape
    - spatial orientation
  2. mineral composition
    - presence and effect of clay minerals
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16
Q

Sedimentary rocks - clastic:

Grain size classification

A

< 0.002 mm Clay

  1. 002 - 0.0063 mm Silt
  2. 0063 - 2.0 mm Sand
  3. 0 - 63 mm Gravel

> 63 mm Boulder

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17
Q

Sedimentary rocks - clastic:

Q,F,L classification

A

Q - quartz
F - feldspar
L - lithoclasts
and matrix

< 5% matrix:

  • > Quartz arenite (Q)
  • > Feldspatic arenite (F,Q)
  • > Lithic arenites (L,Q)

5-50% matrix
Wackes

> 50% matrix:
shales/Mudrocks

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18
Q

Sedimentary rocks - clastic:

Shale

A

mixture of:

clay, silt (some sand) sized particles

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19
Q

Sedimentary rocks - clastic:

Clays - structure

A

alumosilicates with sheet structure and different stacking combinations:

  1. tetrahedral unit with central Si-atom and surrounding O
  2. octahedral unit with central Al and surrounding O atoms and OH groups
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20
Q

Sedimentary rocks - clastic:

Clays - examples

A

Kaolinite (Al)

Illite (K,Al)

Montmorillonite (Ca,Na,Al,Mg,Fe, H2O-layer )

Chlorite (Mg,Al,Fe)

21
Q

Sedimentary rocks - clastic:

Clays - how are exchangeable cations measured ?

A

by cation exchange capacity (CEC)

Smectite/ Montmorillonite HIGH

Kaolinite LOW

22
Q

Sedimentary rocks - chemical:

Carbonates & Evaporate rocks - Formation

A

chemical and biochemical precipitation depending on environments:

  • typically warm
  • shallow
  • clear marine water in low latitudes
23
Q

Sedimentary rocks - chemical:

Carbonates & Evaporate rocks - Sources of secondary porosity

A
  • fracturing
  • solution
  • chemical replacement
24
Q

Sedimentary rocks - chemical:

Carbonates - most abundant carbonate minerals

A
  • calcite CaCO3
  • dolomite CaMg(CO3)2

also:

  • anhydrite
  • chert
  • quartz

+ accessory (phosphates etc.)

25
Sedimentary rocks - chemical: Carbonates - post-depositional processes
dissolution cementation recrystallization dolomitization (increasing porosity) replacement
26
Sedimentary rocks - chemical: Carbonates - Classification after Dunham (Kendall in slides)
Picture in Lecture: Mudstone (mud-supported, < 10% grains) Wackestone (mud-supported, > 10 % grains) Packstone (grain-supported, with mud) Grainstone (grain-supported, without mud) Boundstone (bound at deposition, intergrown, lamination)
27
Texture includes ..
grain size size distribution shape packing
28
What does the grain diameter depend on
particles with non-spherical shape depend on technique of determination 1) sieve analysis: minimum cross-sectional axis 2) image or laser scanning: numerical algorithm for representive size distribution
29
Slide 23: Grain size distribution: | well and poorly sorted
well: mainly one size occur poorly: wide range of different sizes
30
Particle size depend on ..
environmental setting tronsporting agent length and time during transport depositional conditions
31
Phi-scale
phi = -log_2(d) with d in mm
32
median grain size
midpoint at d50 (at 50%)
33
grain sorting S_0
how narrow distribution is: S_0 = (d25/d75)^1/2
34
Skewness S_k
symmetry: S_k = (d25*d75)/d50^2
35
Sieving analysis:
sediment pass through series of stacked sieve meshes (by agitation) wet or dry Sieve catch grains larger than mesh size fractions were weighted o get percentages relative to whole sample
36
Atterberg method
by sedimentation or settling measures rate of sedimentation of particles suspended in liquid not useful for < 5 mikrometer
37
Laser diffraction
measures angular dependence of laser light scattered by particles
38
Stereology mean intercept length of a sphere
3D interpretation of 2D cross sections 0.667 as fraction of diameter was Homework
39
Borehole imaging
1. Optical imaging 2. Acoustic imaging 3. Electrical imaging
40
Borehole imaging 1. Optical imaging
Optical & hyperspectral scanning: - > downhole scanning - > core scanning (360 °) - > 3D Channel Spectral data
41
CT-scanning
use a x-ray source -> through object and scanned by detector on other side numelrical agorithm to construct 2D cross section x-ray attenuation proportional to density determination of porosity
42
Classification of rock properties: direc interest for application (4)
- reservoir properties (porosity, saturation, permeability) - geochemical properties (deformation, strength) - mineralogical characteristics (shale content, fractional min. composition) - content of substances of interest (ore content)
43
Classification of rock properties: measured by geophysical methods
(elastic/seismic, density, electical, nuclear)
44
Scalar properties
- porosity - fluid saturation - density - nuclear cross-sections
45
Tensorial properties
- permeability - deformation modulus - strength properties - elastic, electrical, thermal, magnetic properties
46
Routine core (plug) analysis
- Porosity (photo) - permeability (CT scan) - grain density (fluids) - gamma
47
Special core analysis
- capillary pressure - nuclear magnetic resonance - electrical properties - acoustic properties - clay minerals - specific tests
48
isotropic anisotropic homogenious inhomogenious
isotropic-homogeneous: OOO anisotropic-homogeneous: 000 Isotropic-inhomogenieous: °oO Anisotropic-inhomogeneous: 0o0