Lesson 7: Conglomerates (and Rudites) Flashcards

1
Q

describe and define rudites

A

definition: sedimentary rock composed of gravel sized sediments or 30% clast composition

description: greater than 2mm particle size

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2
Q

2 classifications of rudites

A

sedimentary breccia
conglomerates

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3
Q

two bases rudites are classified on

A

based on:
- percentage between matrix and clasts, and type of matrix
- homogeneity and clast composition

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4
Q

discuss this definition of rudites:
large grain sediments cemented within fine grained matrix

A

“fine grained” can be removed from definition because it is really only infill between large clasts, it is rare for them to be completely absent (in that regard, it cannot be insignificant), but it eventually gets removed after diagenesis

tldr; the matrix is not important because they eventually get removed

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5
Q

2 general subclassifications of rudites when based on the percentage between matrix and clasts as well as the type of matrix

A
  1. grain/clast supported
  2. matrix supported
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6
Q

how many percent of clast composition must a rudite be to consider it grain/clast supported?

A

more than 50%

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7
Q

how many percent of clast composition must a rudite be to consider it matrix supported?

A

less than 50%

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8
Q

special classification of rudites that have more than 85% clast composition

A

orthoconglomerate

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9
Q

what is the requirement for orthoconglomerates (aside from percentage of clasts), what is the implication?

A

the clasts must actually be touching each other, meaning they were supposed to be deposited at the same time

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10
Q

special classification of rudites that have 30% (or 25%) to 5% clast composition

A

paraconglomerate/diamictite

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11
Q

what is the issue with paraconglomerates/diamictites?

A

some authors don’t consider them to be under the rudite group (bc it has very little percentage of clasts)

thus, they can either just be termed:
- mudstone/siltstone/claystone with some gravel sized particles
- conglomeratic mudstone/siltstone/claystone

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12
Q

2 general subclassifications of rudites when based on homogeneity and clast composition

A
  1. polymictic conglomerate
  2. oligomictic/monomictic conglomerate
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13
Q

differentiate the subclassifications of rudites when based on homogeneity and clast composition

A

polymictic -composed of clasts from different sources/mineralogy/petrology

oligomictic/monomictic -composed of clasts from a single source/mineralogy/petrology

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14
Q

expound on the definition of polymictic conglomerates

A

they don’t just mean different rock types, but it also means different composition of rocks.

in other words:
they do not have to be different as in igneous, metamorphic and sedimentary, they can be different as in from different igneous rocks: granite, basalt and diorite

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15
Q

classification of rudites with clasts composed mainly of metastable or unstable minerals

A

petromict conglomerates

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16
Q

why is it that petromict conglomerates are naturally under polymictic, but can also be classified as sometimes not under them?

A

this is because if the minerals/sources/petrology of the clasts are naturally different, that means that there is a big possibility that they are unstable with each other

NOT ALL PETROMICT ARE POLYMICTIC though because minerals from the same source can still be unstable with each other

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17
Q

name the 5(+1) different depositional environments

A
  1. deepwater (deep marine)
  2. shallow marine and coastal
  3. fluvial
  4. alluvial
  5. glacial
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18
Q

examples of deepwater rudites

A
  • basal portions of turbidites
  • olisoliths
19
Q

what are olistoliths?

A

submarine landslide deposits

20
Q

another term for olistoliths

A

olistostrome

21
Q

why are olistoliths considered deep marine deposits when submarine landslides occur on the continental margins?

A

yes, it is true that submarine landslides do occur in shallow marine, but the sediments themselves get deposited eventually at the bottom of the ocean, thus deep marine

22
Q

3 subtypes of environments under shallow marine and coastal

A
  1. wave-worked
  2. wave-, storm-, and current-worked
  3. tide-worked
23
Q

describe the setting of wave-worked environments (3)

A
  • wave energy is sufficient for reworking and transporting sediments
  • sediments tend to be well-sorted and well-rounded
  • seaward dipping
24
Q

explain the reworking in wave-worked environments

A

abrasion, swash and backwash reworks the sediments and sorts them out

25
Q

example of wave-worked environments

A

at beaches, i.e. pebble beach, or that glass beach

26
Q

describe the setting of wave-, storm-, and current-worked environments (3)

A
  • reworking is done by waves, longshore currents and rip currents (also storms)
  • sediments tend to be poorly to moderately sorted (probably bc of the many sources of reworking)
27
Q

explain how tide-worked sediments are formed and how they are recorded

A

they are formed by marine transgression, thus happens over long periods of time (thousands of years). this is why it is often poorly documented (cannot be actually observed), and can only be seen through stratigraphic records

28
Q

tide-worked environments are somewhat related to what other environment?

A

wave-worked environment

29
Q

2 subtypes under fluvial environment

A
  1. sheetflood (shallow braided stream)
  2. stream flow
30
Q

describe sheetflood fluvial environment

A
  • high and episodic energy (floodings)
  • commonly clasts supported with silt or sand matrix
31
Q

describe stream flow fluvial environment

A
  • channelized flow in deeper fluvial channels
  • typically clast supported
32
Q

describe where deeper fluvial channels are exactly

A

downstream, from braided to just before muddy portions (floodplain) that are already purely silt and sand

33
Q

fluvial vs alluvial environments

A

fluvial: river related
alluvial: below the mountain, just out of the mountain

34
Q

describe alluvial sedimentary rocks

A
  • high relief
  • typically coarse grained
  • clast-supported
35
Q

describe the energy change in alluvial environments

A

so basically from steep valleys, there is a sudden change of topography, meaning also sudden change in energy or current. thus the deposits are more sedimentary breccia

36
Q

explain fanglomerates

A
  • debris flow type of deposition
  • may have matrix supported with rapid erosion
37
Q

what are the rudites under glacial environments

A

meltout/lodgement conglomerate/tillite

38
Q

describe meltout/lodgement conglomerate/tillite

A
  • little to no imbrications
  • possibly faceted/striated (from the glacier sliding down the surface)
39
Q

metaconglomerates vs metamorphic conglomerates

A

metaconglomerates: any conglomerate undergoing metamorphism
metamorphic conglomerate: conglomerates with metamorphic origin

40
Q

something to note about when dating rudites

A

date the clasts, not the matrix because they can give different results. it would then be something like the time of formation vs time of burial (clast vs matrix)

41
Q

Aside from alluvial environments, what environment could fanglomerates form? And how?

A

In desert environments: larger particles get eroded immediately along with matrix

42
Q

Aka paraconglomerate

A

Diamictite

43
Q

Sheettflood is aka

A

Shallow braided stream