Strike Energy Limited · ASX:STX

Strike Energy — APPEA Conference Brisbane 2022

17 slides from Strike Energy's conference presentation, May 17, 2022

  1. Slide 1: Reservoir Quality and Diagenesis of the West Erregulla Field, North Perth Basin

    Strike Energy Limited APPEA Conference Brisbane 2022 May 17, 2022 Matthew Wright 1, Andrew Farley 1., Hannah Karena1 and Anthony Cortis 2. 1. Strike Energy Limited, Australia 2. Igesi Consulting, Canada Kingia Sandstone from core at West Erregulla Reservoir Quality and Diagenesis of the West Erregul

  2. Slide 2: Important notice

    Important notice Summary information This document contains summary information regarding Strike Energy Limited (Strike Energy) , its subsidiaries and their respective activities that is current as at the date of this document unless otherwise stated. The information in this document is general in n

  3. Slide 3: Carynginia Structure: Northern Perth Basin

    Carynginia Structure: Northern Perth Basin Kingia/High Cliff Current Well Control (Q1 2022) View from SE Depth in TVDSS • West Erregulla Discovery 2019 : 4563 mTVDSS • West Erregulla Appraisal campaign 2021 : 4605m TVDSS • Post West Erregulla Gas Discoveries : 3 Beharra Springs Deep 3878 mTVDSS– Loc

  4. Slide 4: Kingia Depositional Environment from Petrography

    Kingia Depositional Environment Observations from Petrography Chlorite Rim  Regular currents possibly tidal influence (well sorted laminae, no fine material) Quartz  Chlorite – Forms a continuous layer covering grains  Abundance of quartz grains suggests quartz has been concentrated 4898.71  Dua

  5. Slide 5: Kingia Depositional Environment from Core

    Kingia Depositional Environment Observations from Core The final interpretation based on the core description was estuary fill of an incised valley which was produced by fluvial inclusion during transgression. Characteristics of High Porosity zones 1. Ichnofacies Low diversity and commonly diminutiv

  6. Slide 6: Kingia Depositional Environment

    Kingia Depositional Environment Observations on Image Logs 7 * Source Wilson 2021 – ImageStrat West Erregulla Depositional Model v1.3

  7. Slide 7: Kingia Depositional Environment

    Kingia Depositional Environment Observations on Image Logs 9 * Source Wilson 2021 – ImageStrat West Erregulla Depositional Model v1.3

  8. Slide 8: Kingia Depositional Environment

    Kingia Depositional Environment Observations on Image Logs 10 * Source Wilson 2021 – ImageStrat West Erregulla Depositional Model v1.3

  9. Slide 9: Kingia Depositional Environment

    Kingia Depositional Environment Observations on Image Logs 11 * Source Wilson 2021 – ImageStrat West Erregulla Depositional Model v1.3

  10. Slide 10: Kingia Depositional Environment

    Kingia Depositional Environment Observations on Image Logs 12 * Source Wilson 2021 – ImageStrat West Erregulla Depositional Model v1.3

  11. Slide 11: Kingia Depositional Environment

    Kingia Depositional Environment Observations on Image Logs 13 * Source Wilson 2021 – ImageStrat West Erregulla Depositional Model v1.3

  12. Slide 12: Depth/Temperature Diagenetic Sequence

    Diagenetic Sequence Deposition Time Depth/Temperature Formation of Fe-rich clays Mechanical compaction Clay transformation Quartz cement growth 14

  13. Slide 13: Modern Day Analogue James Bay, Canada

    Modern Day Analogue James Bay, Canada 15

  14. Slide 14: West Erregulla Field

    West Erregulla Field Allanooka High James Bay Canada with West Erregulla Seismic amplitude 16

  15. Slide 15: Summary

    Summary  Recent appraisal drilling within West Erregulla including acquisition of full diameter core has given a greater understanding of the Kingia Sandstone in the Dandaragan Trough.  The initial phase of tidal depositional environment allowed for the mechanism of initial clay coating that in a

  16. Slide 16: Acknowledgments

    Acknowledgments The authors wish to acknowledge Strike Energy Limited and Warrego Energy Limited for permission to publish this material. The authors would also like to acknowledge Andrew Wilson at ImageStrat and JB Peyaud at Fluid Minerals Interactions for their valuable contributions. 18

  17. Slide 17: 19

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