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DTSTART;TZID=Australia/Perth:20251002T180000
DTEND;TZID=Australia/Perth:20251002T200000
DTSTAMP:20260606T043937
CREATED:20250818T062050Z
LAST-MODIFIED:20250905T110143Z
UID:10008718-1759428000-1759435200@pesa.com.au
SUMMARY:PESA WA October Technical Evening:  Three-Dimensional Architecture of Wave-Dominated Delta Deposits
DESCRIPTION:Hosted with thanks to our Platinum sponsor SLB: \n  \n \nGold Sponsors IKON Science: \n \n  \nand Silver Sponsors Delft\, Qeye\, Totum Compliance\, Core Laboratories and Task Fronterra Geoscience: \n                       \n       \n\nPESA WA invites you to our technical evening on Thursday 2nd October.\nSupported by Santos Ltd.\nThree-Dimensional Architecture of Wave-Dominated Delta Deposits\nPresented by Brian J. Willis (Willis Geoscience)\n\nNew numerical wave-influenced delta depositional models are challenging long-held rational for interpreting sea level variations recorded by wave-dominated shallow-marine successions. Shallow-marine\, wave-dominated deposits (parasequences) are generally inferred to exhibit a decrease in wave energy and grain size with increasing water depth and to occur in facies belts that are laterally continuous for long distances along strike. Bedding geometry and vertical facies successions within these parasequences are interpreted in relation to a prograding equilibrium shoreface profile (cf. Bruun rule) and a gradual upward-coarsening facies progression (cf. Walther’s law). Sea-level fall is commonly inferred to generate a sharp-based shoreface succession\, characterized by an abrupt vertical transition from heterolithic lower shoreface to sandy upper shoreface deposits across a marine erosion surface. A truncated vertical shoreface succession\, capped by a marine erosion surface\, is inferred to record significant wave ravinement during sea level rise and transgression. \nThree-dimensional\, process-physics-based\, coupled hydrodynamic-morphodynamic wave-influenced delta models suggest that wave-dominated deltas will develop a sandy shoreface inner clinoform dipping from the subaerial delta plain to a relatively flat wave-scoured subaqueous delta top\, which is laterally separated from a muddier delta front outer clinoform that dips from the subaqueous delta top edge to the shelf floor. As these systems prograde\, deposits of these dual-clinoforms will become vertically stacked and will be separated by a regressive surface of marine erosion formed on the subaqueous delta top. Grain-size contrasts between these vertically stacked clinoform deposits reflect differences in sediment-transport directions and sorting under river- and wave-driven littoral currents along the coast\, and cannot be uniquely related to sea-level changes. Gradual vertical facies successions develop where waves are less effective at reworking river-supplied sediment alongshore. In contrast\, sharp-based shoreface deposits record more effective wave separation of sands onto the shoreface clinoform as muds are preferentially transported offshore onto the subaqueous delta clinoform. \nThe continuity of a regressive surface of marine erosion over many tens to hundreds of kilometres across mid-shelf regions of some stratigraphic sequences reflects a gradual lateral shift in the position of littoral current erosion on a subaqueous delta top. Timelines cross such vertical lithic discontinuities throughout the extent of a prograding deposit\, and the regressive surface of marine erosion thus has little chronostratigraphic significance. The model results are used to suggest: 1) Characteristic strongly asymmetric wave-dominated parasequences suggest common river avulsion at the start of transgression\, 2) Observed down-dip transitions from “gradual-based” to “sharp-based” shoreface deposits might record reduced sediment supply to the coast relative to rates of longshore drift as the system expands toward its auto-retreat limit\, rather than transitions from normal to forced regression\, and 3) Regional “top-truncated” shoreface successions might record progradation of dual-clinoform shorelines with wide deviation in net direction of regional sediment supply and shallow-water wave transport\, rather than significant regional transgressive ravinement. The results of these models suggest caution in inferring sea-level changes from the character of vertical facies changes observed in individual well logs and isolated outcrop exposures. The models suggest new facies relationships that require testing in modern systems\, outcrops\, and subsurface examples. \nTicket Prices:\nMember: $25.00 \nStudent Member: $10.00 \nNon-Member: $50.00 \nStudent Member pricing ends Thursday (1 week prior) at 5pm (AWST). \n 
URL:https://pesa.com.au/events/pesa-wa-october-technical-evening-three-dimensional-architecture-of-wave-dominated-detla-deposits/
LOCATION:The Globe\, 495/497 Wellington Street\, Perth\, Western Australia\, 6000\, Australia
CATEGORIES:Industry,Technical Lunch,WA
ATTACH;FMTTYPE=image/avif:https://pesa.com.au/wp-content/uploads/2025/08/Graphic.avif
ORGANIZER;CN="PESA Western Australia":MAILTO:wa-secretary@pesa.com.au
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=Australia/Adelaide:20251002T190000
DTEND;TZID=Australia/Adelaide:20251002T203000
DTSTAMP:20260606T043937
CREATED:20250521T085005Z
LAST-MODIFIED:20250521T085005Z
UID:10008691-1759431600-1759437000@pesa.com.au
SUMMARY:Field Geology Club Meeting: Sunset Crater\, volcano national monument
DESCRIPTION:We invite you to the Field Geology Club-Hosted Event: \nSunset Crater\, volcano national monument \nSpeaker :Paul Curnow \nPlease note that this event has been organized externally – please reach out to the Field Geology Club for more information: \ncontact@fieldgeologyclubsa.org.au or via their website http://fieldgeologyclubsa.org.au. \nDate: 2nd October 2025
URL:https://pesa.com.au/events/field-geology-club-meeting-sunset-crater-volcano-national-monument/
LOCATION:WA
CATEGORIES:SA / NT,Technical Talk
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=Australia/Perth:20251003T090000
DTEND;TZID=Australia/Perth:20251003T160000
DTSTAMP:20260606T043937
CREATED:20250818T070847Z
LAST-MODIFIED:20251003T001413Z
UID:10008722-1759482000-1759507200@pesa.com.au
SUMMARY:PESA WA - The Mungaroo - Brigadier Depositional System\, Northwest Shelf Australia: A Fluvial-Deltaic Reservoir Core Workshop
DESCRIPTION:Supported by Santos Ltd.\nPESA WA \n3rd October 2025\, 9:00 – 1600 Carlisle Core Library\nThe Mungaroo – Brigadier Depositional System\, Northwest Shelf Australia: A Fluvial-Deltaic Reservoir Core Workshop\nThe Late Triassic Mungaroo and Brigadier Formations in the offshore Northern Carnarvon Basin\, NWS\, Australia\, are the deposits of enormous very low-gradient rivers that fed an intracratonic basin. In such a very low gradient setting\, the rivers expand across a broad distributive deltaic plain\, as sediments spill out of channels into vast interdistributary bays. River distributaries reaching the coast deposit thin\, asymmetrical wave-reworked delta sands. Avulsion of rivers laterally over hundreds of kilometres shifts the locus of deposition\, allowing weak waves and tides time to rework sediments at bay mouths into shoreface sands with tidal inlets. Sea level variations can cause shorelines to shift long distances across these low-gradient alluvial-deltaic plains. \nStandard facies models for fluvial-deltaic systems\, which generally focus on higher gradient settings\, do not provide a suitable template for predicting subsurface facies variations within the Mungaroo and Brigadier deposits. In higher gradient settings\, a river crosses thin delta top deposits to feed a thick\, basinward-thickening deltaic wedge\, with the bulk of river-sourced sediments spread down steep deltaic clinoforms offshore. In very low-gradient settings\, a river loses the competency to carry its sediment load to the coast\, and the bulk of the sediment is extracted on the deltaic plains. Deposits in the expanding network of channels\, on floodplain splays and brackish bay deltas\, and within thin shoreline successions define a unique facies mosaic. \nIn this workshop\, participants can observe the low-gradient fluvial-deltaic facies of the Mungaroo and Brigadier systems in core from the Northwest Shelf of Australia. Brief presentations will introduce conceptual models\, set the stage\, and provide a seismic-scale view of this system. Deposits of the major river in more proximal areas of the system are studied in core from Clio and Saty fields. Lower delta plain and river-dominated bay delta deposits are examined in core from Chandon field. Wave-reworked shoreline deposits will be visible in core from Wheatstone field. Together\, these cores provide a sampling of the facies mosaic deposited by these low-gradient systems. By the end of the workshop\, participants will have gained a better understanding of facies models for low-gradient fluvial-deltaic systems. Mungaroo and Brigadier deposits host world-class hydrocarbon reserves\, which require advanced facies predictions to support subsurface modelling and development predictions. Low-gradient fluvial-deltaic facies are essential components of most shallow marine clastic wedges\, particularly during the early highstand when deltaic systems prograde on top of transgressive shelf deposits. The workshop offers participants a broader perspective on fluvial-deltaic facies models\, extending beyond the standard textbook examples. \n  \nSchedule \n9:00 ─ Safety & Introductions \n9:20 ─ Topic #1: Fluvial deposit architecture defined by process models and concepts (Willis: 20 min) \n9:40 ─ Topic #2: Mungaroo-Brigadier System (Lang: 20 min) \n10:00 ─ Topic #3: Mungaroo fluvial hierarchy and down-basin variations (Payenberg: 20 min) \n10:30 ─ Tea break \n10:45 ─ Start Core #1: Mungaroo fluvial (Clio 2 and Satyr 3) \n11:45 ─ Discussion (core review) \n12:00 ─ Lunch \n12:45 ─ Short topic #1 (20 min plus Q&A) High- vs low-slope systems & asymmetric deltas \n13:10 ─ Start core #2: Chandon 2 (Mungaroo lower delta plain and delta front) \n14:00 ─ 14:15 ─ Tea break \n14:30 ─ Start core #3: Wheatstone 2 BCH1ST1 (Brigadier asymmetric wave-influenced delta) \n15:30 ─ Wrap-up discussion \n15:45 ─ Finish \n16:00 ─ Core store closes \nOrganisers: Dr. Brian Willis (Consultant) Dr. Tobi Payenberg (Chevron) & Prof. Simon Lang (UWA) \nHard limit of 30 attendees.  \n  \nCost:  \nPESA Members:  $250 \nPESA Student Members $100 \n  \nThis event is for PESA WA members only. This is for insurance purposes. Please do not book on behalf of non-members. Please do not attend if you do not have a ticket. \nIf there are any questions\, please don’t hesitate to contact:  wa-secretary@pesa.com.au
URL:https://pesa.com.au/events/pesa-wa-the-mungaroo-brigadier-depositional-system-northwest-shelf-australia-a-fluvial-deltaic-reservoir-core-workshop/
LOCATION:Carlisle core library\, 37 Harris Street\, Carlisle\, WA\, 6101\, Australia
CATEGORIES:Discussion Forum,Industry,WA
ATTACH;FMTTYPE=image/avif:https://pesa.com.au/wp-content/uploads/2025/08/SplashPhoto2.avif
ORGANIZER;CN="PESA Western Australia":MAILTO:wa-secretary@pesa.com.au
GEO:-31.9829615;115.9271201
X-APPLE-STRUCTURED-LOCATION;VALUE=URI;X-ADDRESS=Carlisle core library 37 Harris Street Carlisle WA 6101 Australia;X-APPLE-RADIUS=500;X-TITLE=37 Harris Street:geo:115.9271201,-31.9829615
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=Australia/Perth:20251014T110000
DTEND;TZID=Australia/Perth:20251014T120000
DTSTAMP:20260606T043937
CREATED:20251003T061201Z
LAST-MODIFIED:20251003T061719Z
UID:10008737-1760439600-1760443200@pesa.com.au
SUMMARY:2025 PESA WEBINAR SERIES: Subsurface Focused Fluid Flows (Tayallen Velayatham)
DESCRIPTION:Kindly supported by Rock Flow dynamics  \n  \nThis live webinar will take place at: \n11am | Perth\n12.30pm | Darwin\n1pm | Brisbane\n1:30pm | Adelaide\n2pm | 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. \nSubsurface Focused Fluid Flows\nPresented by Dr Tayallen Velayatham  \nAbstract \n\nSubsurface focused fluid flows are occurrences whereby fluids migrate from deeper to shallower depths through a focusing mechanism\, such as overpressure venting or flow driven by buoyancy drive travelling via permeable migration pathways. Evidence of these phenomena primarily manifest on seismic data as fluid pipes/gas chimneys and pockmarks on surfaces. This presentation will review research completed on this topic and demonstrate how studying these occurrences can provide insight into subsurface fluid dynamics and contribute to better assessing petroleum systems elements.
URL:https://pesa.com.au/events/2025-pesa-webinar-series-subsurface-focused-fluid-flows-tayallen-velayatham/
LOCATION:WA
CATEGORIES:Online
ATTACH;FMTTYPE=image/avif:https://pesa.com.au/wp-content/uploads/2021/09/online-webinar-1.avif
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=Australia/Sydney:20251014T120000
DTEND;TZID=Australia/Sydney:20251014T143000
DTSTAMP:20260606T043937
CREATED:20250918T100104Z
LAST-MODIFIED:20250919T042941Z
UID:10008735-1760443200-1760452200@pesa.com.au
SUMMARY:2025 Acreage Release in the Polda and Otway Basins\, SA
DESCRIPTION:Abstract: \nA key motivation for the South Australian 2025 acreage release is the looming shortfall in energy supply in the southeast Australian market. To facilitate the discovery and production of more gas\, the South Australian Department for Energy and Mining (SADEM) is currently offering prospective acreage in a competitive bid process in two basins (Polda and Otway) across the state.
URL:https://pesa.com.au/events/2025-acreage-release-in-the-polda-and-otway-basins-sa/
LOCATION:Castlereagh Boutique Hotel\, 169 Castlereagh St\, Sydney\, NSW\, 2000\, Australia
CATEGORIES:NSW / ACT,Technical Lunch,Technical Talk
ORGANIZER;CN="PESA New South Wales":MAILTO:pesa.nsw@pesa.com.au
GEO:-33.872562;151.2089734
X-APPLE-STRUCTURED-LOCATION;VALUE=URI;X-ADDRESS=Castlereagh Boutique Hotel 169 Castlereagh St Sydney NSW 2000 Australia;X-APPLE-RADIUS=500;X-TITLE=169 Castlereagh St:geo:151.2089734,-33.872562
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=Australia/Perth:20251016T120000
DTEND;TZID=Australia/Perth:20251016T140000
DTSTAMP:20260606T043937
CREATED:20250827T035147Z
LAST-MODIFIED:20251015T064551Z
UID:10008728-1760616000-1760623200@pesa.com.au
SUMMARY:PESA WA October Technical Lunch: Fault timing and depocentre development in the northern Perth Basin
DESCRIPTION:Hosted with thanks to our Platinum sponsor SLB: \n  \n \nGold Sponsors IKON Science: \n \n  \nand Silver Sponsors Delft\, Qeye and Task Fronterra Geoscience: \n                       \n\nPESA WA invites you to our technical luncheon on Thursday 16th October.\nFault timing and depocentre development in the northern Perth Basin\nPresented by Chris Watts (School of Earth and Planetary Sciences\, Curtin University)\n\nDespite extended periods of exploration in the Perth Basin spanning decades\, the timing of fault activity\, and shifts in depocentre development remain unclear\, especially for intra-basinal faults. Multiple phases of rifting with variable extension directions during the Paleozoic and Mesozoic resulted in a series of predominantly NNW–SSE trending graben and half-graben extending from the Southern Carnarvon Basin in the north\, through the Perth Basin in the south. Two regions of greater structural complexity are indicated by gravity and magnetic data along the margin\, one of which occurs within the northern Perth Basin and the other between sub-basins of the Southern Carnarvon Basin. Recently acquired seismic surveys that better image the pre-Mesozoic stratigraphy in the northern Perth Basin\, paired with legacy seismic and well data have allowed the investigation of fault timing and show a progressive southward shift in fault activity and depocentre location from the late Carboniferous through to the Early Cretaceous\, and that some faults\, despite having different similar orientations\, initiate at different times. Of particular importance is a change in extension direction in the late Triassic and early Jurassic that allowed the development of E-W trending faults. \nTicket Prices:\nMember (Early Bird): $69.00 \nConcession Member [Retired or Hardship]: $59.00 \nStudent Member: $10.00 \nGraduate Member: $20.00 \nNon-Member: $99.00 \nMember (Non-Early Bird): $79.00 \nEarly bird\, Concession\, Student and Graduate Member pricing ends Thursday (1 week prior) at 5pm (AWST). All ticket sales close at 5pm Tuesday (2 days prior). \n 
URL:https://pesa.com.au/events/pesa-wa-june-technical-lunch-fault-timing-and-depocentre-development-in-the-northern-perth-basin/
LOCATION:Parmelia Hilton\, 14 Mill Street\, Perth\, Australia
CATEGORIES:Industry,Technical Lunch,WA
ATTACH;FMTTYPE=image/avif:https://pesa.com.au/wp-content/uploads/2025/08/image_Watts_2-e1756963015650.avif
ORGANIZER;CN="PESA Western Australia":MAILTO:wa-secretary@pesa.com.au
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20251020
DTEND;VALUE=DATE:20251026
DTSTAMP:20260606T043937
CREATED:20250521T084822Z
LAST-MODIFIED:20250521T084822Z
UID:10008692-1760918400-1761436799@pesa.com.au
SUMMARY:Field Geology Club- Excursion: Harlequin Stone and the ancient rocks of northern Yorke peninsula
DESCRIPTION:We invite you to the Field Geology Club-Hosted Event: \nHarlequin Stone and the ancient rocks of northern Yorke peninsula: their geological setting\, origin\, and alteration \nExcursion Leaders: Dr. Colin Conor with Marg Beal and Mandy Bluett \nPlease note that this event has been organized externally – please reach out to the Field Geology Club for more information: \ncontact@fieldgeologyclubsa.org.au or via their website http://fieldgeologyclubsa.org.au. \nDate: 20th-25th October 2025 \n  \n 
URL:https://pesa.com.au/events/field-geology-club-excursion-harlequin-stone-and-the-ancient-rocks-of-northern-yorke-peninsula/
LOCATION:WA
CATEGORIES:Excursion,SA / NT
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20251020
DTEND;VALUE=DATE:20251026
DTSTAMP:20260606T043937
CREATED:20250903T051750Z
LAST-MODIFIED:20250903T051750Z
UID:10008730-1760918400-1761436799@pesa.com.au
SUMMARY:Field Geology Club Excursion: Yorke peninsula
DESCRIPTION:We invite you to the Field Geology Club-Hosted Event \nHarlequin Stone and the ancient rocks of northern Yorke peninsula: their geological setting\, origin\, and alteration \n6-day Excursion \n            Speaker/ Leader: Dr. Colin Conor with Marg Beal and Mandy Bluett \nPlease note that this event has been organized externally – please reach out to the Field Geology Club for more information: \n contact@fieldgeologyclubsa.org.au or via their website http://fieldgeologyclubsa.org.au. \nDate: 20th- 25th Oct 2025
URL:https://pesa.com.au/events/field-geology-club-excursion-yorke-peninsula/
LOCATION:WA
CATEGORIES:Excursion,SA / NT
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20251021
DTEND;VALUE=DATE:20251024
DTSTAMP:20260606T043937
CREATED:20250527T094809Z
LAST-MODIFIED:20250528T040606Z
UID:10008696-1761004800-1761263999@pesa.com.au
SUMMARY:2025 Australian Natural Hydrogen Conference -Adelaide Hills- PESA discount applies
DESCRIPTION:Hundreds of millions of dollars have been committed worldwide to the hunt for natural hydrogen. \nMany more countries and companies are trying to commercialise one of the most abundant and cost-effective forms of hydrogen as the world continues the drive to carbon zero. \nSince the inaugural Natural Hydrogen Association of Australia conference in 2024\, the game has changed. Where are the new natural hydrogen targets; who are the prime movers; what have we learnt from the latest drilling programs; and how have the technical approaches to exploration morphed? \nThis is a fantastic opportunity for interested parties to learn how much closer we are to having at our fingertips a new tool in the carbon zero war. \nThe conference will span 3 days and\, depending on demand\, there could be events on another 2 days. \nThe official conference will begin on Tuesday October 21 with an add-on afternoon workshop on specific technical topics (agenda to be confirmed) and an evening icebreaker session. The official conference is on the Wednesday and Thursday (Oct 22-23)\, with a informal event on the Wednesday evening. \nAs well\, if there is enough demand\, organisers are considering a wine tour of some of the world-renowned wineries of the region on the Monday (Oct 20) and a field trip on Friday (Oct 24). As South Australia is one of the hotbeds of natural hydrogen exploration in this country\, that would be either a core store visit or a trip to one of the sites where natural hydrogen has been identified. \n  \nPESA Member Discounts\nWe welcome interested PESA members to our conference and are offering 10% off the registration pricing. Tickets on sale here: 2025 ANHC. \nYou must be logged in to the PESA website to view the instructions on how to get your discount. \n 
URL:https://pesa.com.au/events/2025-australian-natural-hydrogen-conference/
LOCATION:Adelaide Hills Convention Centre\, 145A Mount Barker Rd\,\, Hahndorf\, SA\, 5245\, Australia
CATEGORIES:Industry,National,SA / NT
ATTACH;FMTTYPE=image/avif:https://pesa.com.au/wp-content/uploads/2025/05/NH2A_col.avif
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=Australia/Perth:20251028T110000
DTEND;TZID=Australia/Perth:20251028T120000
DTSTAMP:20260606T043937
CREATED:20251021T010935Z
LAST-MODIFIED:20251112T021038Z
UID:10008741-1761649200-1761652800@pesa.com.au
SUMMARY:2025 PESA WEBINAR SERIES: 2024 Exploration Year in Review (Sue Slater)
DESCRIPTION:Kindly supported by Rock Flow dynamics  \n  \nThis live webinar will take place at: \n11am | Perth\n12.30pm | Darwin\n1pm | Brisbane\n1:30pm | Adelaide\n2pm | 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. \n2024 Exploration Year in Review\nPresented by Sue Slater \nAbstract \n\nPetroleum exploration expenditure increased both offshore and onshore compared to 2023 numbers\, however this does not equate to a commensurate increase in activity. Onshore jurisdictions dominate the exploration and appraisal activities. In total 82 exploration and appraisal wells were drilled in 2024 (spud date after 31 December 2023). Sixty of these were appraisal wells\, and this was dominated by coal seam gas appraisal drilling in Queensland. Despite the release of the Australian Government’s Future Gas Strategy\, there does not appear to be much in the way of tangible actions to increase exploration. All jurisdictions make land available for exploration via competitive tender\, but in 2024 there were no land releases. Seismic activity in offshore jurisdictions is being limited with new Commonwealth awards being granted without the right to acquire new seismic. Carbon sequestration (CCS) activity continued offshore with the grant of eight of the 2023 land release areas occurring in 2024. While Western Australia\, South Australia and the Northern Territory are taking steps to create the framework for CCS exploration\, in Queensland a sudden announcement saw the cessation of all CCS activity in the Great Artesian Basin\, and importantly also the underlying strata. This ban applies to the use of CO2 in enhanced oil recovery as well. South Australia continues to take lead in natural hydrogen exploration.
URL:https://pesa.com.au/events/2025-pesa-webinar-series-2024-exploration-year-in-review/
LOCATION:WA
CATEGORIES:Online
ATTACH;FMTTYPE=image/avif:https://pesa.com.au/wp-content/uploads/2021/09/online-webinar-1.avif
END:VEVENT
END:VCALENDAR