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DTSTART:20230101T000000
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DTSTART;TZID=Australia/Perth:20240611T110000
DTEND;TZID=Australia/Perth:20240611T120000
DTSTAMP:20260607T111644
CREATED:20240527T013212Z
LAST-MODIFIED:20240527T013212Z
UID:10008588-1718103600-1718107200@pesa.com.au
SUMMARY:2024 PESA WEBINAR SERIES: Possible Compartmentalisation of the Kidson Sub-basin From New Geophysical Data\, and Regional Projects in Western Australia
DESCRIPTION:Kindly supported by Rock Flow dynamics  \n  \nThis live webinar will take place at: \n11am              – Perth\n12.30pm       – Darwin\, Adelaide\n1pm                – Brisbane\, Canberra\, Hobart\, Melbourne\, Sydney \nUse the calendar link on this page to add this event in to your own calendar at the correct local time for your location. \nTickets are free for members (please log in to see this) and $10 for non members. \nPlease buy your tickets and immediately follow the link in the ticket e-mail (not the calendar invite or this webpage\, which is just generic and not event specific) to set up your registration with the webinar software well in advance of the time of the talk. Once registered with the webinar software you will receive a reminder e-mail 1 hour beforehand. \nPossible Compartmentalisation of the Kidson Sub-basin From New Geophysical Data\, and Regional Projects in Western Australia \nPresented by Alex Zhan (DEMIRS; Geological Survey and Resource Strategy Division) \nAbstract \n\nThe Kidson Sub-basin of the southern Canning Basin has long been considered as a relatively simple sag deepening into its depositional axis\, presumably in the central part of the sub-basin. This structural model is based on limited seismic coverage and well intersections near the flanks of the sub-basin\, and is here tentatively revised following integrated mapping with new regional data.  The data integration reveals a possible east-northeast oriented basement ridge with a structural amplitude up to 1000 m in the central part of the Kidson Sub-basin. This ridge possibly divides the Kidson Sub-basin into two distinct parts and potentially is a significant feature with extensive implications for hydrocarbon\, CO2 sequestration\, natural hydrogen\, helium and mineral prospectivities of the sub-basin. Although the basement ridge is supported by regional changes in depositional facies and marginal seismic data\, the existence of such elevated feature remains highly uncertain in the absence of a seismic profile across the ridge. Further work is required to confirm its presence and de-risk exploration efforts.
URL:https://pesa.com.au/events/2024-pesa-webinar-series-possible-compartmentalisation-of-the-kidson-sub-basin-from-new-geophysical-data/
LOCATION:SA
CATEGORIES:Industry,National,Online,Technical Talk
ATTACH;FMTTYPE=image/avif:https://pesa.com.au/wp-content/uploads/2024/01/Figure-e1704624090505.avif
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