Nothing Special   »   [go: up one dir, main page]

Part 8 PDF

Download as pdf or txt
Download as pdf or txt
You are on page 1of 10

AMBIENTES EOLICOS

TEMARIO
• Tipos de dunas
• Clasificación de sistemas eólicos
• Importancia como reservorios
• Icnología
EOLIAN SYSTEMS

Hyper-arid climate regimes

Mountney (2004)
EOLIAN SYSTEMS

Arid climate regimes

Mountney (2004)
EOLIAN SYSTEMS

Semi-Arid climate regimes

Mountney (2004)
ENVIRONMENTS OF ORGANIC
MATTER ACCUMULATION
DESERTS (< 0.05% OM)

• Waxy organic matter


• Almost all converted to CO2 and H2O
• Almost no source-rock potential (but
sandstones in deserts may have high
reservoir potential)
EOLIAN RESERVOIRS

• Eolian sandstones are coarse-grained


and extremely well sorted, so form
good reservoir rocks.
• They need an external source of
hydrocarbons to become a reservoir.
• Evaporites may form caprocks.
AMBIENTES EOLICOS
• Icnodiversidad y densidad baja o
raramente moderada
• Dominio de trazas de locomoción, con
presencia subordinada de estructuras de
habitación y alimentación
• Asociación de trazas de invertebrados
(mayormente artrópodos) con huellas de
vertebrados

ICNOLOGIA
BIBLIOGRAFIA
• Brookfield, M.E. 1992. Eolian systems.
In: Walker, R.G. & James, N.P. (eds.),
Facies Models. Response to Sea Level
Change. Geological Association of
Canada, p. 143-156.
• Mountney, N.P. 2004. The sedimentary
signature of deserts and their response to
environmental change. Geology Today
20: 101-106.

You might also like