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Thrust BeltsBarcelona, Spain
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Carbonate ComplexityNaples, Italy
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BEOS 2022London, England
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Black Sea Super BasinsTrabzon, Turkey
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Mixed/Hybrid SystemsLisbon, Portugal
Field Seminar
Barcelona, Spain
Saturday, 11 June Sunday, 12 June 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
Barcelona, Spain
Monday, 13 June Tuesday, 14 June 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, 15 June Thursday, 16 June 2022, 8:00 a.m.–5:00 p.m.

Field Trip Leader: Jaume Vergés Limit: 20 Participants The main plan of this fieldtrip to the South Pyrenean Fold Belt is to have an overview of a fold belt and adjacent foreland basin through four well-exposed and well-known localities. Each example permits the discussion of different geological processes related to the interplay between tectonics and sedimentation and the role of salt-tectonics during both pre-compression rifting and during tectonic inversion. Day 1 - Wednesday 15 June 2022 Stop 1: Overview of the southern margin of the Ebro foreland basin: Montserrat fan-delta The main objective In the Montserrat fan-delta locality is to characterize the evolution of the southern margin of the Ebro foreland basin during the Pyrenean shortening with especial emphasis on its tectono-sedimentary evolution through the Eocene. The size and quality of this outcrop is directly comparable to good seismic examples. Stop 2: Role of detachment levels and salt-tectonics in building the fold belt: Cardona diapir The main objective in the Cardona diapir locality is to provide an overview of salt tectonics in compressional settings at different scales using the South Pyrenean examples. The role of pre- and syn-orogenic evaporitic levels during shortening in fold belts is discussed as well the interplay between tectonics and sedimentation. Overnight in Solsona Day 2 - Thursday 16 June 2022 Stop 1: 3-D Growth strata to define folding mechanisms and growing topography: Sant Llorenç de Morunys In the Sant Llorenç de Morunys locality. along the footwall of the Pyrenean thrust sheets, we can observe the 3-D views of the large-scale and best preserved growth strata worldwide; several square kilometres and more than 500 m of tectonic relief. The size and quality of this outcrop is directly comparable to good seismic examples. Stop 2: Evolution and inversion of a salt-related rift basin: Roca Narieda In the Roca Narieda locality we discuss the role of pre-orogenic salt tectonics in development of salt-related rift basins and their control on Lower Cretaceous platform growth. Outcrop is also superb and is directly comparable to good seismic examples. Drive to Barcelona (2:30 hours) Notice: In mid-June the weather is rather hot and therefore it is recommended to bring fresh clothes, hat or cap and sunscreen as well as drinking water. Do not forget suitable hiking boots. If weather conditions are good we can walk on steep terrain for short distances (but only in two of the four localities).

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American Association of Petroleum Geologists (AAPG)
Field Seminar
Naples, Italy
Tuesday, 21 June 2022, 8:00 a.m.–5:00 p.m.

Field Trip Leaders: Alessandro Iannace Stefano Tavani Mariano Parente (University of Naples Federico II, Italy) Fee: £150 Participant Limit: Min. 10 - Max. 20 Themes The Cretaceous platform carbonates of the Sorrento Peninsula offer wonderful outcrop analogues for the reservoirs of the Monte Alpi and Tempa Rossa oil fields of subsurface Basilicata and for fractured carbonate reservoirs of other Tethyan carbonate systems. During this 1-day field trip we will see how the facies, diagenetic characters and stacking patterns of cyclical Barremian-Albian inner platform carbonates controls mechanical stratigraphy and fracture distribution. We will look at the fracture network at different scales, from stratabound fractures to reservoir-scale fracture corridors, combining panoramic observations of subvertical cliffs of the Mt. Faito ridge, exposing a >300m thick stratigraphic interval, with detailed observations of the same beds along roadcuts. Then, we will move to a road cut near Positano where we will observe a small-scale intraplatform basin, developed in Aptian-Albian carbonates, focusing on soft-sediment deformation, organic-rich dolostones, fault-zone architecture and breccia bodies. Itinerary and Stops Transfer from Naples to Mt Faito by minibuses (about 1h drive) Stop 1 – Ticciano village: general introduction to the geology of the southern Apennines and to the Apennine Carbonate Platform; panorama of the Mesozoic platform carbonates of the Monte Faito ridge Stop 2 – Croce dell’Eremita roadcut: facies and fracture distribution of Barremian-Albian inner platform interbedded dolostones-limestones Lunch Stop 3 – Santa Maria del Castello: panoramic view of Monte Conocchia cliff: distribution and arrest of vertical through-going joints and fracture corridors in a seismic scale carbonate platform exposure Stop 4 – roadcut north of Positano: middle Cretaceous synsedimentary tectonics, soft sediment deformation, organic-rich dolostones and breccia bodies in a small intraplatform trough. Driving back to Naples (about 90min drive)

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American Association of Petroleum Geologists (AAPG)
Workshop
Naples, Italy
Wednesday, 22 June Thursday, 23 June 2022, 8:00 a.m.–5:00 p.m.

Modelling carbonate sequences and reservoirs has always been a challenging task. Carbonate rocks are generated and subsequently modified by a large variety of biological, physical and chemical processes that start at the time of deposition and end today. To unravel the geological evolution and history of carbonate sequences is fundamental not only for understanding their hydrocarbons potential but also for their role as potential reservoirs for renewable energy (geothermal) or geological gas storage (CO2 and hydrogen). Several science disciplines are often involved to fully understand the characteristics of carbonate rocks and old approaches and new technologies and tools are nowadays applied in these types of sequences. The objective of this meeting is to allow scientists and engineers working on carbonate rocks in academia and industry to share their most recent experience, work, approaches and use of innovative technologies to increase the understanding of the very complex world of carbonates.

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American Association of Petroleum Geologists (AAPG)
Field Seminar
Naples, Italy
Friday, 24 June Saturday, 25 June 2022, 8:00 a.m.–5:00 p.m.

Field Trip Leaders: Jean Borgomano – CEREGE, Aix-Marseille Université, France Michele Morsilli – University of Ferrara, Italy Fees: €450 + VAT Fee Includes: Transportation during the field trip Overnight Accommodation Breakfast, lunch 2 days and dinner Themes The Gargano Promontory (southern Italy) offers the opportunity to investigate a complete carbonate facies transect from inner platform to basin and to reconstruct the various events that shaped and controlled the evolution of the Apulia Carbonate Platform during the Cretaceous and Paleogene. This area can be considered a wonderful outcrop analog to better understand and visualize facies, depositional geometries, stratigraphic relationships and to compare them with other carbonate platforms. The exposed carbonate rocks show well-preserved original reservoir properties and form relevant analogues of subsurface reservoirs located in different structural settings; e.g. inner platform palaeokarst (Ombrina Mare, Rospo Mare oil fields), subthrust setting (Monte Alpi, Tempa Rossa), slope, base-of-slope resedimented carbonate facies (Elsa, Miglianico, Aquila, Rovesti), as well as relevant for the comparison with the specular Adriatic Carbonate Platform (AdCP) or other Tethyan carbonate systems. Main goals of this field trip are the observation of the facies and stratigraphic architecture of the inner platform and of slope and base-of-slope units deposited during the Early - Late Cretaceous and Eocene, as well as the carbonate production and exporting/resedimentation processes. The Apulia Carbonate Platform represents a well-known case study of a carbonate platform with different evolution through time. Facies distribution from inner platform to base-of-slope, stratigraphic architecture and depositional geometries, together with retreat and drowning of the platform or margin collapses, and seismic-scale outcrops, in a relatively poorly deformed context, constitute a text book examples of a Cretaceous Carbonate System. Itinerary and Stops Day 1 Naples (or Bari airport) to Apricena by bus (travel about 3 h) Stop 1.1 - Apricena quarries district: stop on peritidal cycles of Lower Cretaceous, fractured and karst reservoir (outcrop analog of the Rospo Mare oil field). Lunch Stop 1.2 - Belvedere di Ruggiano: stop on scalloped/faulted platform margin of mid-Cretaceous and base of slope to basin facies associations. Night in Monte Sant’Angelo Day 2 Stop 2.1 Monte Sant’Angelo: slope to basin facies of the Lower Cretaceous and facies observation of the resedimented succession of the Upper Cretaceous. Lunch Stop 2.2 Monte Sant’Angelo to Manfredonia road – Upper Cretaceous slope to base of slope facies and architecture of the systems. Stop 2.3 (optional) - Monte Saraceno-Mattinata: panoramic view of the Upper Jurassic-Lower Cretaceous sequence and Valanginian retreating/drowning of the Apulia Platform and depositional geometries of the Eocene clinoforms. End of the Excursion (travel to Naples or Bari airport)

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American Association of Petroleum Geologists (AAPG)
Industry Meeting
London, England
Wednesday, 29 June Thursday, 30 June 2022, 8:00 a.m.–5:00 p.m.

London 2022 will build on the success of the SEAPEX conference held in April 2019 in Singapore and the PESGB-SEAPEX London 2018 event in highlighting the resurgence of E&P interest in Asia-Pacific with new ideas, new plays and new successes. Join us in London on 29-30 June 2022.

American Association of Petroleum Geologists (AAPG)
Industry Meeting
London, England
Thursday, 1 September Friday, 2 September 2022, 8:00 a.m.–5:00 p.m.

A truly global event focused on prospecting, business transaction and deal making for the oil and gas E&P sector - for prospects, properties, products, service providers, investors and all decision-makers necessary to close a deal.

American Association of Petroleum Geologists (AAPG)
Workshop
Trabzon, Turkey
Tuesday, 6 September Wednesday, 7 September 2022, 8:00 a.m.–5:00 p.m.

Join us in Trabzon, Turkey, for "Exploration and Production in the Black Sea Region and Super-Basin Thinking" a AAPG Europe Geoscience Workshop to be held on September 6-7, 2022.

American Association of Petroleum Geologists (AAPG)
Workshop
Lisbon, Portugal
Thursday, 18 May Friday, 19 May 2023, 8:00 a.m.–5:00 p.m.

This 2-day conference brings together diverse experts working on modern and ancient turbidite, MTDs, contourite and hybrid/mixed systems in order to improve the present-day knowledge, models and predictive power.

American Association of Petroleum Geologists (AAPG)
Online Training
 
19 August 2010

This presentation will show where there are cases of missing sections, but none of them can be attributed to normal faulting.

Tulsa Oklahoma USA AAPG 19 August, 2010 19 August, 2010 1462 02 December, 2013

Region Office Contacts

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