• 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

Bass Basin geology and petroleum exploration

17/12/1986 by Sharperedge

Bass Basin geology and petroleum exploration

 

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: Second South-Eastern Australia Oil Exploration Symposium - Technical Papers

Authors: G.C. Smith

Date Published: December 1986

Number of Pages: 41

Reference Type: Book Section

Abstract:

The Bass Basin is an intracratonic rift basin located offshore between Victoria and Tasmania. The tectonosedimentary history is controlled by Otway rifting between Australia and Antarctica and to a lesser extent by Tasman Sea rifting. A Lower Cretaceous volcanogenic synrift sequence (Otway Group) and a Tasman
Sea Cenomanian to Santonian shale dominated synrift sequence (Durroon Formation), occurring in large tilted fault blocks, are recognizable on seismic. These are overlain by a post-rift sequence comprising a Campanian to Eocene non-marine coal measure sequence (Eastern View Group) and a marine sequence (Demons Bluff Formation and Torquay Group) which drowned and filled the basin during its sag phase with shallow-water mudstones, marls and carbonates.
The burial history records the effects of rapid subsidence, sedimentation and low T -P metamorphism in the rift and early post-rift phases, waning in the Tertiary. The rift sequences are confined to a narrow NW-SE basin axis and exhibit the highest metamorphic ranks except on basement highs. The post-rift sequences onlap the older sequences and basement rocks extending over the basin margins, and range from lower ranks on the margins to moderately high ranks at depth along the basin axis. Maturation in the Eastern View Group is mainly controlled by the Cretaceous to Eocene burial. The exinite organic matter is mature only at depth along the basin axis being immature on the basin margins, whereas the vitrinite and inertinite are mature or overmature throughout most of the basin.
The Upper Eastern View Group has good reservoirs, seal and source rocks but lacks structure and is low in
maturity. The Lower Eastern View Group has good intraformational seals and reasonable structure but poor source rocks and poor reservoirs. Overall the Bass Basin has a low probability for discovery of large commercial oil or gas fields and only a moderate probability for discovery of small commercial oil or gas fields.

Tags: basin Bass exploration geology petroleum

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