Inferred Lithology - Prediction

Slides:



Advertisements
Similar presentations
What Is Seismic Facies Analysis?
Advertisements

Astronaut photo of Delta
Seismic Stratigraphy EPS 444
Deltaic Depositional Systems
The relative age of rocks and geological events.
HYDROCARBON PETROLEUM SYSTEM
Sedimentologi Kamal Roslan Mohamed DELTA.
Deltaic Depositional Systems
Marginal Marine and Open-Shelf Environments
 The specification says:  Describe the deposition in deltaic environments of delta top (topsets) to form coal, sandstones of the delta slope (foresets)
Sand Bodies Lowstand Deltas
Professor Chris Kendall
Geological Modeling: Deterministic and Stochastic Models
Depositional Environments, Facies, Facies Models and Paleogeograpy Geologic History in Three Dimensions.
Part 8 ALLUVIAL FANS and DELTAS. Classic alluvial fan. Fans often develop where confined channels on steep gradients suddenly emerge from their canyons,
Features of depositional environments
Lateral Lithostratigraphic Changes
Remote Sensing Lab, Part B Patterns of Deposition.
Geological map of Leeds area
Depositional Environments and Sedimentary Facies
Important Stratigraphic and Geomorphic Concepts Facies.
Deltas and Estuaries.
Regional Geology of Khwisero District, Kenya April 2012 Scott Patterson.
Using Well Logs (e-logs) in the Petroleum industry Earth Science World.
The Stratigraphic Record
Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis Dr. Tark Hamilton Dr. Tark Hamilton Readings from the Holy Book of Tark: (6:1-26) Readings from.
Geology 1023 Environments & Facies. Sediments are being deposited in various locations simultaneously Conditions vary from place to place –Medium –Speed.
Sedimentary Geology Geos 240 – Chapter 8 Depositional Environments Part 3 Deltas & Continental Shelves Dr. Tark Hamilton Dr. Tark Hamilton Readings from.
The Tools of Subsurface Analysis
Log Correlation Correlation can be defined as the determination of stratigraphic or structural units that are equivalent in time, age or stratigraphic.
Interpreting Ancient Environments
= coastal plain (rivers + floodplain) = tidal marsh = lagoon
Facies and Facies Models. What is a facies? A sedimentary unit with consistent characteristics (lithology, grain size, texture, structures, etc.) that.
Malikah Patel1, Daniel Mikeš2
Department of Geology and Geological Engineering
Delta Environments Nile Delta Mississippi Delta.
Stages of River Development
Unit 2: Introduction to Sequence Stratigraphy
by Aitor A. Ichaso, and Robert W. Dalrymple
Combining statistical rock physics and sedimentology to reduce uncertainty in seismic reservoir characterization Per Åge Avseth Norsk Hydro Research Centre.
Seismic Facies Analysis
Step 3: Resistivity Logs
of these basic elements
The Container Reservoir Trap Seal
Department of Geology, University of Dhaka Maps and Map Reading Lab.
Step 1: Lithology Using the Gamma Ray log, define a shale base line
Outline Review causes of seismic response
Seismic attribute applications:
What Is Seismic Facies Analysis?
Seismic Interpretation
Seismic - Units 10s of Meters Thick
The Convolution Method
Transgressions and regressions: the key to Earth history
Stratigraphic Traps – Sub-Unconformity & Reef
Thud! Ring! Seismic Response What causes a seismic response?
How Can We Define Stratal Units?
How to Correlate these Logs?
Example: Nearshore Sands
Lithostratigraphy Well A Well B Well C Well D Coastal Plain Datum
A Geologic Model 1m 75 m Perm 250 mD Sand Shale 0.1 mD 50 m Slide 16
Sedimentary Rocks A sedimentary rock is formed by the accumulation and compaction of sediments (rock pieces, minerals, animal parts, or chemical precipitates)
by D. J. Went, R. V. Hamilton, N. H. Platt, and J. R. Underhill
Lithostratigraphic Interpretation
Why Is That ??? Recall: Reflections are generated where there is a change in acoustic properties (z =  * v) Consider: Where would sharp changes in.
Well Log Correlation Well logs give us detailed information at the location of the borehole If there are several wells in an area, we can correlate stratigraphic.
Seismic Facies Mapping Exercise
Vertical Resolution Gamma Ray
Controls on marginal marine and nonmarine stratigraphic architecture:
Well Correlation Exercise
Geology 1023 Environments & Facies.
Presentation transcript:

Inferred Lithology - Prediction Facies Model Delta Front Sandstone Delta Front Siltstone Pro-Delta Shales Offshore Clay Sea Level Prediction Crevasse Splay Channel Fill Proximal Distributary Mouth Bar Distal Prodelta Delta Front SLIDE 14 Given these interpreted EODs, we can think about the types of depositional bodies we should have We use depositional models based on modern analogues, ancient outcrops and/or laboratory experiments If we were to drill in the marginal marine (yellow) area of the map on the last slide, we would expect (top-down) Delta front sands Delta front silts Prodelta shales Offshore clays We can even anticipate a vertical (and lateral) facies succession as shown on the right We can even use geo-statistics to predict, for example, the thickness and lateral extent of channel sands or crevasse splays Courtesy of ExxonMobil L 11 – Stratigraphic Analysis