Lecture 12 - Diagenesis Flashcards

More notes needed on the last few slides

1
Q

What is diagenesis

A

The chemial and phsyical processses which act upon sediment grains in the subsirface” they give way to metamorphism but there is no clear line

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2
Q

Diagenitc processe: compaction

A

massof overlying sediment, water squeezed out and sediment compacted together

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3
Q

Process recrystalisation

A

Unstable minerals change to their crystal forms

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4
Q

Dissolution

A

Unstable minerals may dissolve

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5
Q

Replacement

A

Usntale minerals may be replaces

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6
Q

Authigenesis

A

Precipitation of new minerals within pores

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7
Q

Cementaion

A

Sediment cemeted by authgetic precipitaion

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8
Q

bacterial action

A

degradation of organic matter

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9
Q

where can we look at diagensis

A

mudrocks
sandstones
carbonates

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10
Q

Diagenesis in mudrocks, main process?

A

The main diagentic process is Compaction

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11
Q

effect on thickness of mudrock

A

it can be compacted up to ten times

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12
Q

effects of explusion of water on mudrocks

A

At despotion mudrocks are 70% water, at depths of 1km they are 30%, much iof the water here is locked up. at 100km heat is also needed for the desaturation of these mudrocks

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13
Q

What are the changes in the clay minerolfy

A

The main change is

smectities + potassium -> illites + water

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14
Q

When does this smectities change happens

A

2-3km deep and 70-90degrees C

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15
Q

Sandstone diagensis what can efect it

A
depositional enviroment
sediment comp
sediment texture
pore water chem
burial and uplift histrory
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16
Q

Properties of sand compared to mud (water props)

A

the sediment grains in sand such as quartz are not as ductile and therefore not ductile under temps and pressures

17
Q

what are the four factors that compation of sandstone depends on

A

1) clay content ( average is 5%)
2) Perecenatge of ductile grains (such as mud most sandstones only contain 15% of non ductile materials)
3) sorting of the sand grains
4) burial depth (pressure)

18
Q

What forms concavo convex contacts

A

If one grain dissolves preferintally

19
Q

What forms sutured contacts

A

if grains are of a similar soulbitlty

20
Q

What are the four main cements in sandstones

A

1) quatz
2) calcite
3) haematite
4) clay mineral cement

21
Q

Quatz cement proprs

A

Pressure-solution can provide silica in the system for cermentss

22
Q

calcite cement properties

A

Calcite cements can redissolve if acidic water passes through them.

23
Q

Haematite cement

A

Most of the iron is supplied as a sissoultion of other rocks. only a tiny amount is needed to make the rocks RED (IRON Fe2O3)

24
Q

Clay cement props

A

Most modern sands have little caly matrix. etiher clay matrix is primary or the clay matrix is diagentic

25
Q

Diagensis in carbontaes info

A

Begins as soon as the carbonate is precipatated or deposited. alage sponges worms etc bore into the carbonate

26
Q

Cemenation in limestone

A

cemenation is the main diagentic process that turns loose sediment into hard limestone

27
Q

what are hard grounds

A

Typically when sedimenation has ceased for 1000s of years

Crusts on the sediment surface

28
Q

explain stylo bites

A

These are sutured surface which cut grains, cements and matrix as a result of chemicak compation