Seds refs Flashcards

1
Q

Structures

A

Mike Leader, 2011

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2
Q

Skewness

A

M Tucker 2001
A measure of the symmetry of the distribution of grain size and sorting
• +0.3 = strongly fine skewed to -0.3 = strongly coarse skewed
• Reflects the depositional environment
o Beach sands have a negative skew because finer components are carried off by wave action
o River sands are positively skewed as the silt and clay is not removed by currents but is trapped between larger grains
• In general sediment becomes more negatively skewed and finer grained along its transport path

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3
Q

Compaction

A

Bjørlykke 2013
Grain size, shape and sorting, both in sandstones and mudstones, play an important role in determining the mechanical compaction prior to chemical compaction
Also temps for chemical compaction
- 90-130 for quartz over growth
- 60-80 for calcite cement
- 80-90 illite
Fawad (2010) – poorly sorted sediments are more resistant to mechanical compaction

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4
Q

Evaporites

A

Leader, 2011
Although several periods during the Phanerozoic have been marked by impressive occurences, e.g. opening of the Atlantic and the Red Sea ocean basins, and desiccation of the Miocene Mediterranean

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5
Q

Alluvial fans

A

Iran - Zagros Mountains and fault zone
Jones - 2013 - This study has demonstrated that although tectonism can induce fan development, it is the sensitive balance between aridity and humidity resulting from changes in the climate regime of a region that influences the nature of fan sequences and how they interrelate to associated fa- cies. This is easily overlooked in the need to identify tectonic events and interpret ancient basin history

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6
Q

Deep ocean seds

A

Leader 2013
Ocean floor above the CCD = biogenic calcareous oozes dominate - cocolithophore
Ocean floor below CCD = red clay

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7
Q

Controls on seds

A

Jones 2103 - The concept of autocyclic and allocyclic controls on sedimentation and stratigraphy, emphasizing the climatic variable - Allocyclic vs autocyclic controls
Humphrey and Heller (1995) – Perturbed by allocyclic tectonics and climate but use autocyclic to stay in equilibrium

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8
Q

Pebble Clusters

A

Renzo DalCin (1968)

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