--> Using Paleoclimate Models to Predict Source Rock Occurrence: Results from the GANDOLPH Project, by Christopher Scotese, John Zumberge, Harold Illich, Thomas Moore, and Scott Ramos, #40287 (2008)
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Using Paleoclimate Models to Predict Previous HitSourceNext Hit Previous HitRockNext Hit Occurrence: Results from the GANDOLPH Project*

By

Christopher Scotese1, John Zumberge2, Harold Illich2, Thomas Moore3, and Scott Ramos4

 

Search and Discovery Article #40287 (2008)

Posted May 30, 2008

 

*Adapted from oral presentation at AAPG Annual Convention, San Antonio, Texas, April 20-23, 2008.

 

1 Earth & Environmental Sciences, Univeristy of Texas at Arlington, Arlington, TX ([email protected])

2 GeoMark Research Ltd., Houston, TX

3 PaleoTerra Inc, Bollingbrook, IL

4 Infometrix inc, Bothell, WA

 

Abstract

Understanding the temporal and spatial distribution of Previous HitsourceNext Hit rocks, especially in unexplored and under-explored frontier regions is one of the greatest challenges in hydrocarbon system analysis. In order to address this problem, GeoMark Research Ltd, together with the PALEOMAP Project and PaleoTerra Inc., for the past 3 years has been building a GIS atlas of plate tectonic, paleogeographic, and paleoclimatic maps that illustrate the paleoenvironmental setting of known Previous HitsourceNext Hit rocks and oils (GANDOLPH Project). Eight of 12 planned intervals have been completed:

  • Mid-Miocene
  • Cenomanian/Turonian (C/T)
  • Early Cretaceous
  • Late Jurassic
  • Late Triassic
  • Early Permian
  • Late Devonian
  • Latest Ordovician-Early Silurian

One of the principal research goals of the GANDOLPH Project has been to test the paleoclimatic predictions made by the paleoclimate simulations with information about Previous HitsourceNext Hit Previous HitrockNext Hit paleoenviornmental conditions obtained from biomarkers in the oils. A second major research goal of the project has the construction of a tool (Previous HitSourceNext Hit Rocker) that uses multivariate statistical techniques to:

  • Identify the kinds of paleoenvironments in which Previous HitsourceNext Hit rocks are likely to have formed, and
  • Estimate the reliability of these Previous HitsourceNext Hit Previous HitrockNext Hit predictions.

In this presentation we shall briefly review the results from all eight time intervals, and then discuss, in detail, the results from the C/T (Cenomanian/Turonian) and Late Devonian simulations. We shall describe how we built the SourceRocker tool and shall review the predictions it has made regarding the occurrence of probable Previous HitsourceNext Hit rocks in unexplored, and under-explored frontier regions.

 

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uGRANDOLPH

uAnalogs & controls

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uAbstract

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uGRANDOLPH

uAnalogs & controls

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uAbstract

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uGRANDOLPH

uAnalogs & controls

uWorkflow

uConclusions

 

What is GRANDOLPH?
Previous HitSourceNext Hit Previous HitRockNext Hit Prediction Methodology using an Earth Systems Approach

Project Objectives

  • Provide plate reconstructions for 18 geologic time slices
    • (Year 1: C/T, EPerm, Lt Jur, Lt Dev)
    • (Year 2 : ECret(2), Trias, ESil, Oligo-Mio)
    • (Year 3: MEoc, EJur, ECarb, Late Neoprot)
    • (Year 4: Olig, K/T, P/Tr, SiluroDev, EOrd)
  • Produce paleoclimatic and paleo-oceanographic simulations for each time slice (FOAM)
  • “Evolve” predictive criteria relating geography, climate, and ocean state to hydrocarbon Previous HitsourceNext Hit bed deposition (SourceRocker)

 

What Would You Like to know?

 

Previous HitSourceNext Hit Previous HitRockNext Hit Analogs for Exploration Prospects

  • Probability of Previous HitSourceNext Hit Previous HitRockNext Hit Occurrence
  • Previous HitSourceNext Hit Previous HitRockNext Hit Type
  • Previous HitSourceNext Hit Previous HitRockNext Hit Richness
  • Previous HitSourceNext Hit Previous HitRockNext Hit Thickness

Previous HitSourceNext Hit Previous HitRockNext Hit Controls

  • Productivity
    • Upwelling (Marine)
    • Terrestrial Organic Input
  • Preservation
    • Anoxic & Suboxic
      • poor vertical mixing
      • restricted conditions
  • Dilution

 

GRANDOLPH Workflow

  • Build Paleogeography (PaleoDEM) CS
  • Compile Global Previous HitSourceNext Hit Previous HitRockNext Hit data HI
  • Run Climate Model (FOAM) TM
  • Classify OILS & Previous HitSourceNext Hit Rocks HI & JZ
  • Find Associations between OILS and Climate Results and Paleogeographic parameters JZ
  • Use Environmental “FingerPrint” to Predict Previous HitSourceNext Hit Previous HitRockNext Hit Analogs CS

 

Conclusions

  • A global, Phanerozoic database of Previous HitsourceNext Hit rocks and paleo-Previous HitsourceNext Hit Previous HitrockNext Hit environments has been assembled
  • Previous HitSourceNext Hit Rocks form in environments that have a specific “Earth Systems Fingerprint”
  • This Fingerprint can be used to identify other possible areas with Previous HitsourceNext Hit Previous HitrockNext Hit potential
  • The “Previous HitSourceNext Hit Finder” program uses multivariate techniques to identify Previous HitsourceNext Hit Previous HitrockTop analogs
  • A prototype of “SourceFinder” is up and running

 

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