• Member Login
  • |
  • Join Now
PESA - Energy Geoscience

Promoting Professional and Technical Excellence in Energy Geoscience – Networking, On-going Professional Education, Monthly Technical Meetings

  • Home
  • About
    • About PESA
    • Objectives
    • PESA History
    • PESA Affiliates
    • Constitution and Rules
    • Strategic Plan
  • Events
    • Online
    • NSW / ACT
    • QLD
    • SA / NT
    • VIC / TAS
    • WA
    • Industry
    • Social
    • Past Events
  • Membership
    • Join Us
    • APPEA Conference Discounts
    • AEGC 2025 Travel Bursaries
    • PESA Membership Awards
  • Latest News
    • All News
    • Feature Articles
    • Industry
    • Company Updates
    • Tech Talk (public)
    • PESA Branch Activities
  • Library
    • Technical Library
    • PESA Gazette
    • Webinars
    • PESA News Magazine
    • Knowledgette Recordings
  • Scholarships
  • Employment
    • View Job Opportunities
    • Submit Job
  • Contact

Constraints on the hydrocarbon charge history of sandstone reservoirs in the Strzelecki Field, Eromanga Basin, South Australia

16/12/2004 by Sharperedge

Constraints on the hydrocarbon charge history of sandstone reservoirs in the Strzelecki Field, Eromanga Basin, South Australia

 

Download Section

Please log in to download this file.

Alternatively, you can search for this item and individually purchase it from the PESA collection at AAPG DataPages

PESA collection at AAPG DataPages

Publication Name: PESA's Eastern Australasian Basin Symposium II

Authors: L. Kramer, D.M. McKirdy, K.R. Arouri, L. Schwark and D. Leythaeuser

Date Published: December 2004

Number of Pages: 31

Reference Type: Book Section

Abstract:

The Strzelecki oil and gas field is located on the southern margin of the Nappamerri Trough, a major hydrocarbon
kitchen in the Cooper/Eromanga petroleum province of central Australia. Its oil-bearing sandstones (Hutton, Birkhead, Namur) are all of Mesozoic age. With a view to reconstructing their respective charge histories, core plugs of each reservoir at Strzelecki-4, 5 and 6 were extracted in a high-pressure solvent flow-through cell. This device sequentially recovers individual oil charges from the intact pore systems of a reservoir rock, in the reverse order of their arrival at the trap. Initial extraction with dichloromethane retrieves the oil that is freely mobile in the pore network ('free oil' = final charge). The subsequent chloroform/methanol extracts represent the part of the oil that is immobile due to adsorption on pore walls ('adsorbed oil'= initial charge) or retained in smaller, less accessible pores.
The residual oils exhibit systematic variations in yield and bulk composition within each oil column. A minor upward decrease in thermal maturity (-0.02-0.03% R,) is evident in the Hutton and Namur oil pools. However, at any given level, there is generally no significant difference in either maturity or source affinity between the 'free' and 'adsorbed' oils. On a larger scale, the 'free' oils display a field-wide maturity differential: Hutton, 0.87%; Birkhead, 0.86%; and Namur, 0.94% R,. In terms of their source affinity, the relative Araucariacean input is Birkhead> Hutton> Namur. All three oil pools comprise mixtures of intra-Jurassic (probably Birkhead) and Permian hydrocarbons. The major contribution (65-80%) appears to have come from source rocks in the Toolachee Formation of the underlying Cooper Basin.

Tags: Biomarkers chargehistory. CooperBasin. EromangaBasin. in-reservoir mixing migration residual oil solvent flow-through extraction

PESA - Energy Geoscience

PESA Energy Geoscience is a non-profit association of individuals involved in the exploration of oil and gas.

Connect with us

Subscribe to our newsletter and stay on the loop of what is happening in the field of Energy Geoscience and events near you.

pesa newsletter
* indicates required

PESA Energy Geoscience will use the information you provide on this form to be in touch with you and to provide updates and marketing. Please confirm you give us permission to contact you via your email address:

You can change your mind at any time by clicking the unsubscribe link in the footer of any email you receive from us. We will treat your information with respect. For more information about our privacy practices please visit our website. By clicking below, you agree that we may process your information in accordance with these terms.

We use Mailchimp as our marketing platform. By clicking below to subscribe, you acknowledge that your information will be transferred to Mailchimp for processing. Learn more about Mailchimp's privacy practices.

Copyright © 2025 PESA - Energy Geoscience. All Rights Reserved.

  • Advertise
  • Contact
  • Policies
  • Privacy
  • Terms & Conditions