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Exploration and Production in the Black Sea Region and Super-Basin Thinking Call for Abstracts
Expires in 11 days
Methods used by large companies to target marketing to individual consumers are being applied in the search for energy and mineral resources.
Unconventional resources represent a bright opportunity for the United States' economic and energy future, but that is in no sense guaranteed. A misinformed public debate about the impacts and merits of hydraulic fracturing in particular and the oil industry in general threatens that future.
Heightened creativity. Enhanced problem-solving and decision-making. Improved risk management. These are just some of the benefits of diverse workplaces, according to panelists for a special session at the AAPG International Conference and Exhibition.
Cindy Yeilding of BP America discusses the production history and geology of one of the world’s most prolific hydrocarbon super basins.
Can super basins save the planet? IHS Markit, the international industry analysis firm, estimates the world will need to replace production of more than 14.5 billion barrels of oil equivalent annually by the year 2040.
Understanding the business side of oil and gas exploration and development is fundamental to success, especially in times of uncertainty and disruptive technologies. Welcome to an interview with Joe Dumesnil, Overland Oil and Gas. Joe will be speaking at the AAPG Annual Convention in the Special Session on the Business of Oil and Gas.
The second edition of the AAPG Stratigraphic Traps of the Middle East workshop took place on 11 – 13 December 2017 at the Shangri-La Barr Al Jissah hotel, Muscat, Oman. This year we had seventy two attendees from ten different countries.
The industry might be tempted to relax or postpone environmental compliance activities, especially those that might be new or expensive. Succumbing to this temptation is risky and could prove more costly in the long run.
Groups such as Greenpeace, the Sierra Club and Food & Water Watch are harnessing the power of fear tactics and social media to spread falsehoods and misinformation in order to rally large groups of citizens to join their forces and put money in their coffers. And, they are becoming increasingly successful.
The fourth edition of the AAPG/EAGE 'Tight Reservoirs in the Middle East” GTW took place on 27 – 28 November 2018 at the Downtown Rotana Hotel, Manama, Bahrain. This year we had 80 attendees from ten different countries.
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.
This short course will comprise lectures, short exercises and discussion sessions. The course will focus on a number of case studies that link outcrop and subsurface geology and have relevance to petroleum exploration and production. Case studies range from Silurian to Miocene in age and come from North African and Mediterranean Basins. The course builds on basic knowledge of sedimentary geology but does not require specialist skills from participants.
This presentation gives a short overview of Time-lapse (4D) seismic potential over a few case studies from TotalEnergies’ portfolio of assets. It shall begin with a brief introduction of basic concepts of 4D seismic; some of TotalEnergies’ 4D seismic related activities over the years as well as an overview of some published methods and workflows on 4D seismic. Some examples of application of 4D seismic in clastic and carbonate fields, as well as its use in a geomechanical context will be given, and finally conclude with a reflection that 4D is a transverse subject where many disciplines are involved.
The structurally complex area of Northern Tunisia (onshore and offshore) corresponds to a fold and thrust belt (FTB) zone, a result of the tertiary compressional/trans-pressional tectonics (Pyrenean and Alpine). This field trip will focus on the different structural styles in the different segments of the area using a rich amount of outcropping and subsurface data and their relationships within the petroleum systems components (source rock and reservoir Rock).
Field Trip Leaders:
Jean Borgomano – CEREGE, Aix-Marseille Université, France
Michele Morsilli – University of Ferrara, Italy
€450 + VAT
Transportation during the field trip
Breakfast, lunch 2 days and dinner
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
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).
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
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.
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)
Field Trip Leaders:
(University of Naples Federico II, Italy)
Min. 10 - Max. 20
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
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)
Join us for a workshop where experts will explore the Carpathian foreland and the Dnieper-Donetsk rift basins with a focus not only on hydrocarbons, but the utilization of geothermal resources, hydrogen exploration and CCUS.
Date: 25 September 2022
Time: 8:30am - 4:30pm
Course Instructor: Alberto Ortiz, Net Zero Carbon Solutions
Registration Fee: $530
Registration Deadline: 25 August 2022
Short Course registration is included as part of the GTW registration process.
The petrophysical characterization of unconventional shale-type reservoirs has been one of the most approached and relevant issues in the oil and gas industry in the last 8 years. This is because after several years, the operating companies comprehended the impact that an appropriate characterization of the reservoir has on their project economics.
Another reason for this were the technical obstacles encountered in the measurement of petrophysical properties such as porosity, saturation and permeability due to the complexity of this type of reservoir. Obstacles and limitations not only relate to laboratory measurements but also to electrical logging tools.
As a consequence of this, nowadays, petrophysical evaluations in this type of reservoir do not have standardized workflows established and accepted worldwide as is the case for conventional reservoirs. This motivates the professionals involved in the study of this type of rocks to dedicate a lot of effort in the validation of the technologies used, and sometimes it is difficult for them to understand the results, the evaluation of uncertainties and the construction of petrophysical models with results and representative parameters of the subsurface conditions.
This course will focus on providing key knowledge for a better characterization of the rock both in the aspects related to the matrix represented by mineralogy and kerogen as well as the fluids present. The approach will be based on the convergence of different technologies that support and give robustness to the results.
The contents that will be provided will include laboratory testing techniques and petrophysical evaluation of electrical well logs for unconventional shale-type reservoirs. The contents provided will cover a variety of studies based on the most diverse physical principles that will include the latest advances and techniques used in the industry such as Nuclear Magnetic Resonance, Spectroscopy, Dielectric, Computed axial tomography and SEM images, among others.
As a result of this, attendees will have tools that allow a more comprehensive understanding of this type of rocks, a better assessment of the uncertainty of the model used and the necessary steps to improve its precision, accelerating the learning curve. The contents provided will also allow knowing the critical parameters that must be taken into account for the definition of areas to be drilled.
Reservoir heterogeneity characterization from outcrops to lab data and electrical logging.
Most relevant unconventional plays of the world. Main characteristics.
The petrophysical model. Components and definitions, construction, uncertainties, strengths and weakness.
Lab studies: porosity, saturation, mineralogy, organic geochemistry and permeability.
Electrical logging response on unconventional shale plays: triple combo, NMR, NMR T1T2, nuclear spectroscopy, spectral GR, dielectric.
The effect of maturity on kerogen.
Challenges on water saturation calculation.
Data integration. Interpretation workflows and core calibration.
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.
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.
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)
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
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 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.
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. -->
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.
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.
The workshop aims to provide a comprehensive understanding of the source rocks in the Middle East. The technical program is developed in a way that coves the depositional environments and transport processes, basin modeling and detailed rock characterisation including geochemisty, geomechanics and petrophysics.
This is a less-technical education topic. It can be condensed to an hour or given as 2 two-hour sessions. It stresses selected controversial aspects of fracking that touch some combination of environment and economics and includes a short video of how fracking is done.
Request a visit from David Weinberg!
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