Lecture 7 - Facies Models Part II Flashcards

1
Q

What are aeolian desposits?

A

this is where incoming radiation heats the lower lats and takes mositire from here and moves it to the high lats, meaning a dry arid enviroment such as a desert

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2
Q

what is sandblasting?

A

Grains move just above the sediment surface by saltation colliding with toher grains

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3
Q

What is sandblasting effects on pebbles?

A

Sand blasting gives pebbles curbed or straight sides theses are called Ventifacts

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4
Q

What is the most common desert mineral

A

Quatz

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5
Q

What else occours here?

A

microscopic pitting and frosting

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6
Q

What is the sorting and rounding of these sand grains

A

Well rounded and well sorted

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7
Q

Wind transport properties

A

Wind is obvsiously much less dense than water so a really strong wind is needed to transport size grains.

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8
Q

What does this wind form

A

Dunes, either around obstacles forming two dunes then the weak eddies allow the dunes to grown to form one large sand dune.

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9
Q

explanation of sanddune migration

A

Sand dues are eroded or the windward side and deposited on the lee slope. Successive slip faces make for cross bedding.

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10
Q

Techtonic setting for sand dunes

A

Inland basins, 10-30defrees or behind mountain rain shaddows

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11
Q

Geometry of sand dunes

A

Thick tabular bodies can go for 100s of km

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12
Q

Sedimentolofy

A
Enormous cross cut beds
some mud cracked shales
desert pavement gravles
well rounded
quatx rich
no fine matrix
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13
Q

Fossils?

A

Rare footprints, insect burrows

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14
Q

What do these cross cut beddings in the rock record indicate

A

Past wind directions

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15
Q

Deltas explaination

A

Sedimenty desposits at river mouths, deltas prograde (build out)

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16
Q

What are the three types of deltas

A

Small, Lobate, elongate

17
Q

One delta can contain three enviorments, what the they?

A

Delta plain, delta front, prodelta

18
Q

Techtonic setting of a delta

A

Passive margins and subsiding basins

19
Q

Geometry of a delta

A

Roughly tirangluar plans

Wednge shape in cross section

20
Q

Sedimentology

A

Coarse sand to fine mud, sometimes coal ripples and cross bedded sandstones

21
Q

Fossils

A

Organic matter common in interdistribuaty areas

22
Q

Preitidal envroiments explainations

A

found between high and low tide, found in costal regions where river sediments < marine eriosin, Unlike prograding deltas, sediment in peritidal environments is reworked by tides

23
Q

Peritidal tectonic settings

A

passive margin with shallow coastal regiions

24
Q

Geometry

A

Tabular, local sand bodies paralell to shorine

25
Q

Sedimentology

A

Sand and mud cracks, hering bone cross cutting bedding

26
Q

Fossils?

A

Oysters, plant remans and algea mats