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During the last glacial maximum (LGM), the Antarctic ice sheets expanded, reaching the shelf break in many places, including in the Antarctic Peninsula (AP); since the end of the LGM (~14,000 years ago) ice has retreated back to its current position, leaving a suite of subglacial geomorphic features on the seafloor. Sedimentary archives sequestered in deep fjords have formed under marine conditions, recording the ongoing glacial retreat and climatic fluctuations.

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Sequence stratigraphy is an evolving field that has thus defied all attempts at formalization. Part of this resistance to stability is because central assumptions core to the science maintain scrutiny and occasionally undergo either modification or full refute.

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The generation of point bars by lateral accretion during lateral expansion and downstream translation of river meanders is a well described process, and a primary means for generation of sandy bar reservoirs within fluvial strata. Further examination of this process in modern and ancient settings points, however, to a wide variation on this simple theme.

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During times of past extensive glaciations, the Antarctic ice sheet extended from its current position, reaching across the continental shelf. As the ice sheet retreated to its modern extent, the shrinking ice sheet left behind seawater, rather than ancient ice, leaving behind a sedimentary signature of deglacial history.

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The linkage of process to stratigraphic expression is based primarily upon the observation that modern depositional patterns replicate in the ancient. Uniformitarianism implies that this commonality in pattern translates to a commonality in causal mechanism.
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Channel belts are the principle reservoirs in fluvial systems. The degree to which these belts are merged or separated is a critical determiner for reservoir volumes. The degree to which reservoirs within belts are connected is equally critical.

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The New Madid seismic zone (NMSZ) is the second highest risk area for earthquake hazard in the United States. Its fame arises from a cluster of at least three great earthquakes during the winter of 1811/1812 that shook most of the North American continent. A repeat of these earthquakes would deeply impact the mid-continent region and potentially be devastating to the nearby cities of St. Louis and Memphis.

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The Antarctic continent, which is nearly completely covered by a thick ice sheet, and the surrounding ocean with its fringing belt of sea-ice, ice shelves and drifting icebergs, offer challenges to geological investigations that seek to unravel the history of one of Earth's last frontiers.

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A seismic interpretation study of reflection profiles was undertaken to identify sedimentary and structural components of the tectonic development of the West Greenland continental margin. The new structural framework reveals a long and complex tectono-stratigraphy and evolution.

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In the coming year, the Energy Minerals Division is looking to improve and expand its information delivery system. EMD also is seeking volunteers to fill a number of vacant section and region councilor positions.
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In-Person Training
Muscat Oman 18 January, 2016 20 January, 2016 16517 Desktop /Portals/0/PackFlashItemImages/WebReady/gtw2016me-hydrocarbon-seals-hero.jpg?width=100&height=100&mode=crop&anchor=middlecenter&quality=75amp;encoder=freeimage&progressive=true Subsalt Traps, Structural Traps, Stratigraphic Traps, Diagenetic Traps, Fractured Carbonate Reservoirs, Reservoir Characterization, Engineering, Seismic Attributes, Geochemical Fingerprinting, 3D Seismic, Sedimentology and Stratigraphy, Sequence Stratigraphy, Evaporites, Clastics, Carbonates, Structure, Fold and Thrust Belts, Compressional Systems, Geomechanics and Fracture Analysis, Production, Drive Mechanisms
Muscat, Oman
18-20 January 2016

This workshop has the primary goal to share knowledge, case studies, techniques and workflows pertaining to the understanding and prediction of hydrocarbon seals for exploration and production in the Middle East. These seals range in age from Pre-Cambrian to Tertiary.    

Abu Dhabi United Arab Emirates 25 January, 2016 26 January, 2016 16518 Desktop /Portals/0/PackFlashItemImages/WebReady/gtw2016me-source-rocks-hero.jpg?width=100&height=100&mode=crop&anchor=middlecenter&quality=75amp;encoder=freeimage&progressive=true Geochemistry and Basin Modeling, Source Rock, Development and Operations, Engineering, Conventional Drilling, Directional Drilling, Infill Drilling, Clastics, Sedimentology and Stratigraphy, Conventional Sandstones, Petroleum Systems, Fluvial Deltaic Systems, Structure, Compressional Systems, Extensional Systems, Sequence Stratigraphy, Stratigraphic Traps, Petrophysics and Well Logs, Basin Modeling, Oil and Gas Analysis, Reservoir Characterization
Abu Dhabi, United Arab Emirates
25-26 January 2016

This three-day workshop aims to provide a forum for professionals from industry, academia and government agencies, who are actively involved in the study of Middle Eastern Source Rocks, to share their advances in source rock related fields, present their experiences and challenges, and demonstrate relevant technologies and solutions.

Lagos Nigeria 22 February, 2016 24 February, 2016 21922 Desktop /Portals/0/PackFlashItemImages/WebReady/sequence-stratigraphy-concepts-principles-applications-clastic-depositional-environments-02feb-2016-hero.jpg?width=100&height=100&mode=crop&anchor=middlecenter&quality=75amp;encoder=freeimage&progressive=true Engineering, Reservoir Characterization, Geochemistry and Basin Modeling, Source Rock, Petrophysics and Well Logs, Sedimentology and Stratigraphy, Clastics, Conventional Sandstones, Deep Sea / Deepwater, Deepwater Turbidites, Eolian Sandstones, Estuarine Deposits, Fluvial Deltaic Systems, High Stand Deposits, Incised Valley Deposits, Lacustrine Deposits, Low Stand Deposits, Marine, Regressive Deposits, Sheet Sand Deposits, Shelf Sand Deposits, Slope, Transgressive Deposits, Sequence Stratigraphy, Deep Basin Gas, Diagenetic Traps, Stratigraphic Traps, Structural Traps
Lagos, Nigeria
22-24 February 2016
Sequence stratigraphy provides a framework for the integration of geological, geophysical, biostratigraphic and engineering data, with the aim of predicting the distribution of reservoir, source rock and seal lithologies. It gives the geoscientist a powerful predictive tool for regional basin analysis, shelf-to-basin correlation, and characterization of reservoir heterogeneity. This course will examine the underlying geological principles, processes and terminology related to sequence stratigraphic interpretation. The strength of this course is the application of these basic principles to subsurface datasets in a series of well-founded exercises.
Online Training
10 May, 2012 10 May, 2012 1486 Desktop /Portals/0/PackFlashItemImages/WebReady/oc-es-genetic-sequences-in-eagle-ford-austin.jpg?width=100&height=100&mode=crop&anchor=middlecenter&quality=75amp;encoder=freeimage&progressive=true
10 May 2012

Recognition and Correlation of the Eagle Ford, Austin Formations in South Texas can be enhanced with High Resolution Biostratigraphy, fossil abundance peaks and Maximum Flooding Surfaces correlated to Upper Cretaceous sequence stratigraphic cycle chart after Gradstein, 2010.

17 February, 2011 17 February, 2011 1469 Desktop /Portals/0/PackFlashItemImages/WebReady/oc-es-siliclastic-sequence-stratigraphy.jpg?width=100&height=100&mode=crop&anchor=middlecenter&quality=75amp;encoder=freeimage&progressive=true
17 February 2011

This presentation is designed for exploration/production geologists and geological managers or reservoir engineers.

14 February, 3000 14 February, 3000 7817 Desktop /Portals/0/PackFlashItemImages/WebReady/oc-es-generic-hero.jpg?width=100&height=100&mode=crop&anchor=middlecenter&quality=75amp;encoder=freeimage&progressive=true
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