Title: Lecture 15 Lithostratigraphy
1Lecture 15 Lithostratigraphy
2Stratigraphy Putting together the whole picture
(processes and history)
- Lithostratigraphy
- Biostratigraphy
- Seismic stratigraphy
- Magnetostratigraphy
- Geochemistry
- stable istopes
- radiometric dating
3I. Facies (Steno, 1669) aspect or
appearance
Can be genetic (fluvial facies) or descriptive
(sandstone facies)
Lithofacies a consistent lithologic character
within a formation. E.g. an evaporite lithofacies
Walthers law (1894) facies that occur in
conformable vertical successions of strata also
occur in laterally adjacent environments.
4Transgressions and regressions, progradations
5Classical interpretation of a cyclothem
6Assymetry in transgressive and regressive
deposition
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8II. Accumulation
- Base level. Above sealevel, preservation is the
exception rather than the rule - Sediment traps
- tectonic
- basin subsidence
- sea-level rise
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10III. Gaps
- Diastems obscure, small gaps in the record.
Barrell (1917) - Unconformities larger gaps in the record.
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15IV. Correlation
- Demonstrating the equivalence or correspondence
of geographically separated parts of a geologic
unit
16Old (pre-1930) and new interpretations of units
in the Devonian Catskills. Layer-cake versus
concept of facies change.
17An example of time-transgression of lithofacies
from the Everglades
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20V. Sequences
- Major unconformities representing Earths broad
tectonic or eustatic events.
21Sloss (1963)
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23VI. Time, Time-Rock and Rock Units
- Time (geochronologic) units
- Eon
- Era
- Period
- Epoch
- Age
- Time-rock chronostratigraphic) units
- Eonothem
- Erathem
- System
- Series
- Stage
- Zone
24Examples
- Time units
- Phanerozoic eon
- Cenozoic era
- Quaternary period
- Holocene epoch
- Wisconsinan age
- Time-rock units
- Eonothem
- Erathem
- System
- Series
- Stage
25Rock (lithostratigraphic) units
- Supergroup
- Group
- FORMATION a mappable unit with distinctive
lithic characteristics - Member
- Bed