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IMAGE 2021Denver, Colorado
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Fracture Concepts
Abstract Submission Deadline 01 December, 2021
Tectonic GeoscienceSydney, Australia
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Thrust BeltsBarcelona, Spain
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EvaporitesVirtual Event
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Salt TectonicsVirtual Event

Upcoming Events

Short Course
Saturday, 25 September Sunday, 26 September 2021, 8:00 a.m.–5:00 p.m.

This is a hands-on class anchored with a 65-piece teaching collection of natural and induced fractures in core that students will work with during class exercises. The class provides insights into fracture mechanics and the origins of fractures, and uses those concepts in a very applied sense to instill an understanding of natural fractures and their potential effects on permeability and fluid flow.

American Association of Petroleum Geologists (AAPG)
ACE
Denver, Colorado
Sunday, 26 September – Friday, 1 October 2021, 8:00 a.m.–5:00 p.m.

The Society of Exploration Geophysicists (SEG) and the American Association of Petroleum Geologists (AAPG), along with Society for Sedimentary Geology (SEPM) are excited to introduce, IMAGE ‘21 – the International Meeting for Applied Geoscience & Energy. This combination of multiple disciplines across the geosciences sector has created a single powerhouse event that will deliver the latest applied-geoscience insights, technology, and training. Make plans to join geoscientists from around the globe, 26 September–1 October 2021, in-person at the Colorado Convention Center and online

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American Association of Petroleum Geologists (AAPG)
Workshop
Virtual Workshop
Monday, 18 October Wednesday, 20 October 2021, 10:30 a.m.–6:00 p.m.

Join us virtually in this event that was due to be hosted in Salzburg, the “castle of salt” and cradle of Mozart and Doppler. We aim to host an interactive meeting aimed at bringing together different perspectives in the science of evaporite basins: from their formation to their deformation, from description and characterization to modelling. Exploratory success in evaporite-rich basins worldwide has depended on the role of evaporites as a deformable substrate, as a seal, or even as a good thermal conductor. The aim of this workshop is to improve our understanding and predictive ability by addressing evaporite systems in an integrated manner, all the way from precipitation to structuration, and exploring the multiple properties of evaporite sequences. This will be done via technical sessions, keynote speaker presentations, panel sessions and more!

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American Association of Petroleum Geologists (AAPG)
Field Seminar
Virtual Field Seminar
Monday, 18 October 2021, 6:30 p.m.–8:30 p.m.

Dates: Oct. 18th 18:30-20:30 CET Location: Virtual within Google Earth Included: KMZ files for use in Google Earth Technical Requirements: High speed internet connection Google Earth installed This field trip will take you from Salzburg to the UNESCO World Heritage Site of Hallstatt, where salt has been exploited for 5000 years and where we will take a look at the interaction of salt diapirism with syn-tectonic sedimentation. The impact of the Hallstatt diapir on our understanding Alpine orogenesis will be discussed. You will also be given a brief overview of the spectacular Bronze Age mine galleries of Hallstatt! This is an interactive field trip! You will guide yourself to the outcrops from the comfort of your desk. Anybody wishing to participate in this pre-conference field trip (Oct. 18th) needs to have access to a computer with GoogleEarth installed. KMZ files (total size of hundreds of MB) will be distributed prior to the field trip via download link to all participants. It will be the participants' responsibility to show up to the field trip with these files downloaded and open in GoogleEarth. During the field trip, we will access the internet to visualize 3D models in Sketchfab; a suitable browser and good connection speed are also required. Please test beforehand on any Sketchfab model.

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American Association of Petroleum Geologists (AAPG)
Workshop
Barcelona, Spain
Monday, 28 March Tuesday, 29 March 2022, 8:00 a.m.–5:00 p.m.

This workshop brings together experts from academia and industry from a range of disciplines to share experiences, new approaches, new data and new ways of integrating information that can help in reducing the uncertainties related to the exploration activities in Thrust Belt Systems.

American Association of Petroleum Geologists (AAPG)
Field Seminar
Barcelona, Spain
Wednesday, 30 March Thursday, 31 March 2022, 8:00 a.m.–5:00 p.m.

Trip leader(s): Josep Anton Muñoz, Pablo Granado and Eduard Roca Limit: 20 Participants The aim of this 2-day field trip is the recognition of the key structural features of a fold and thrust belt detached on salt that has resulted from the inversion of a previous passive margin. To achieve this objective, some of the key and most spectacular localities of the southern Pyrenees have been selected along the ECORS-Pyrenees transect. This is a reference cross-section provided that for many years a huge amount of geological and geophysical data sets has been collected and integrating into a kinematic model of the South-Pyrenean fold and thrust belt. Subsurface data (well logs and seismic sections) will be combined with field observations. One of the main characteristics of the southern Pyrenees is the preservation of the synorogenic sediments since the earlier stages of deformation, which not only provide time constraints but also allow us discussion of kinematics of fault-related folds and thrust systems. Finally, the mild contractional deformation permits deciphering the initial geometry of the rift system and the salt structures that configure the structural grain of the passive margin before the inversion, allowing discussion of the role that these structures play during the fold and thrust belt development. Itinerary: (day by day details of the trip) Day 1 Stop 1.1: The South-Pyrenean thrust front. Sant Llorenç de Montgai Structure of a frontal thrust system and related unconformities. Out of sequence thrusts and synorogenic sediments. The frontal thrust system of the South-central Pyrenees has been detached into the Triassic evaporites and involves a thin Mesozoic succession. It is characterized by an emergent thrust system during the sedimentation of upper Eocene and lower Oligocene continental sediments. Frontal thrusts were progressively buried by conglomerates, triggering a break-back thrusting sequence and the development of out-of-sequence thrusts bringing together strongly different Mesozoic successions, such as the Montroig thrust in the picture. Stop 1.2: The Ager basin and the Montsec thrust sheet. Fontllonga The Ager basin in the footwall of the Montsec thrust. The Montsec thrust sheet developed from the Paleocene to the Early Eocene as recorded by continental to shallow marine sediments deposited in its footwall (Ager basin) as well as in the Tremp-Graus piggy-back basin. The lower Eocene sediments of these basins grade westward into the slope succession filling the Ainsa basin at the footwall of the Montsec thrust. Stop 1.3: The frontal structure of the Montsec thrust sheet. Ametlla (optional: Montrebei) Fault-propagation fold related with the inversion of Early Cretaceous extensional faults and growth deltaic sediments in the footwall syncline. The Montsec thrust sheet involves the northern part of the Upper Cretaceous foreland basin characterised by a strong subsident turbiditic trough at the footwall of the Bóixols thrust. These turbidites grade southward into a carbonatic platform that constitutes the backbone of the Montsec Range (main ridge and cliff of the pictures). Underneath the Upper Cretaceous carbonates, some Early Cretaceous extensional faults are preserved in the hanging wall of the Montsec thrust, but others have controlled the development of a hanging wall frontal anticline. The geometry of this anticline as well as the structure of the growth sediments in the footwall Ager syncline are visible in the field. The subthrust geometry will be discussed integrating surface observations and the available seismic and well data. Overnight in Tremp Day 2 Stop 2.1: The Sant Corneli-Bóixols anticline Inversion of the rift margin The Sant Corneli-Bóixols anticline is the most prominent frontal structure of the Bóixols thrust sheet in the central Pyrenees. This fold trends east–west and crops out for greater than 40 km along strike. The Sant Corneli-Bóixols anticline involves a thick Mesozoic succession detached on top of Triassic evaporites. The prefolding sequence consists of up to 5 km of prerift, synrift, and postrift carbonates ranging in age from Jurassic to Upper Cretaceous. Synfolding Upper Cretaceous sediments start with the upper Santonian carbonates and continue with a succession of Campanian and Maastrichtian marls and turbidites. The Sant Corneli–Bóixols anticline is an example of an inversion fold developed along the rift margin of the Lower Cretaceous basin. Its geometry is related with the inverted extensional system. In particular, the three-dimensional geometry, including the saddles between culminations, is inherited from the previous transfer faults of the segmented rift margin. Available seismic data and 3 exploratory wells constrain the geometry at depth. Stop 2.2: The synororgenic Paleogene conglomerates Inverted Lower Cretaceous basin and Eocene-Oligocene synorogenic conglomerates at Collegats gorge. Stop 2.3 (optional): The Sopeira and Aulet minibasins. Sopeira Minibasins developed by extensional collapse and salt evacuation during the thermal subsidence at the southern Pyrenean rift margin. Inversion of these mini-basins at the early stages of Pyrenean contractional deformation during Late Cretaceous. Additional logistic information Transportation Transportation will be with a small bus, assisted by minivans to have access to some of the outcrops. Physical demand, equipment and safety This is an easy field trip with very easy and limited hikes to get to the outcrops. Outcrops will be from main sealed roads. Safety vests will be available, to be used by everybody of the group wherever required and asked to. There will be First Aid Kits available in each car during fieldwork. Climate The climate during mid-end November in the fieldwork area can be cold and rainy, although dry and sunny days may occur as well. The temperature for November in Tremp can range between 30C and 170C. Participants should be prepared in case we should encounter bad weather and you should bring warm and waterproof clothes and suitable hiking boots. -->

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American Association of Petroleum Geologists (AAPG)
Workshop
Sydney, Australia
Wednesday, 6 July Thursday, 7 July 2022, 8:00 a.m.–5:00 p.m.

As we transition to a new commercial reality for our industries, there has never been a more important time for Earth Scientists to take a seat at the table. This workshop is designed to share our knowledge of the petroleum sector with other branches of the geosciences, while learning from their experiences. Join us for this hybrid online and in-person workshop on 6 July 2022.

American Association of Petroleum Geologists (AAPG)

Deadlines

Headquarters Contacts

Susan Nash
Susan Nash Director, Innovation and Emerging Science and Technology, breeling 4053147730