Week 2 Flashcards
(33 cards)
Stratigraphy =
Study of vertical sequence of strata and lateral variations of individual beds on a regional basin
- stratum
- bedding planes (bounding surfaces)
Sharp boundaries represent
Period of non-deposition
Lithostratigraphy =
Study of PHYSICAL relationship among rock units
Biostratigraphy (concept)
:) Shorter lifespan = more precisely correlated
:) Rapidly evolving
:) Broad distribution
e.g. Graptolites, lower Palaeozoic correlate to 100,000 year time frame
Chemostratigraphy (concept)
U/Th/K
Gamma rays, consistent with certain lithologies
- low for sand, high for mud
Allostratigraphy =
Uses discontinuities:
- unconformities
- omission surfaces
- ravinement surfaces
- flooding surfaces
Ravinement surface =
Erosional!
1st surface due to flooding (increasing SL)
Flooding surface =
Separates young/old and obvious change in SL
Facies =
Distinctive packet of sedimentary rock with specific sedimentary features FROM DEPOSITIONAL ENVIRONMENT
e.g. “deltaic” facies
Lithofacies =
Based on grain size/mineralogy
Biofacies =
Based on fossils
Walthers Law =
Concept that vertical succession of facies represents lateral changes in environment
What controls accommodation space?
SEA SURFACE
- eustasy = global SL from datum
SEA FLOOR
- tectonics
RATE OF SEDIMENT ACC
Sea level falls =
Sea cuts down and incises
Regression
Coarsening upwards/prograding sequence
Foreshore material steps over and works its way towards the sea
Sea level rises =
Sediment deposited further up near river
Transgression
Fining upwards sequence
Mechanisms of SL change
Varying ice volume (global/regional)
Varying ridge volume
- slow spreading = decrease (steeper = more vol so requires “more sea”
- fast spreading = increases
Tectonic effects
- plate convergence
- continental collision
Systems tracts =
Heterogeneous sedimentary units produced by contemporaneous depositional systems during specific phases of basal level variation
TST
Transgressive
Increase in SL
RST
Regressive
Decrease in SL
Parasequence =
~conformable succession of genetically related beds/bedsets bounded by marine flooding surfaces and their correlative surfaces
Together form a sequence with unconformities as boundaries
Progradational parasequence
Decreasing SL
Aggradational parasequence
Static SL
Retrogradational parasequence
Increasing SL
Subaerial unconformity =
Formed through subaerial exposure and erosion including downcutting rivers/soil/karst processes