The Vital Role of Mudstone/Shale Studies in Advancing Sequence Stratigraphy in General
Speaker: Kevin M. Bohacs, KMBohacs Geoconsulting

 Webinar 

February 17, 2021
11:00 am-12:00 pm Mountain Time 
The GoToWebinar link will be emailed two days in advance of the webinar. 

Webinar pricing
CSPG member: $30.00 +gst 
Non-member: $45.00 +gst

Please note: Registration closes February 16 at 12:00 pm Mountain Time 

ABSTRACT 
Studies of mudstone/shale have benefitted from using the sequence-stratigraphic approach but have also improved sequence stratigraphy as a discipline. Observations accumulated over the last 35 years, accelerated by the ‘shale-gas revolution’, indicate that mud is a quite active component of depositional systems at many scales and not just passive fill among coarser grains. It appears that various grain-size classes each have their own inherent geometry and the stratal record is the resultant of vigorous interaction among the grain sizes. The influences of mud range from being essential to many sediment-transport mechanisms at the bed scale to forming distinctive types of parasequences and complex stratal geometries at depositional-sequence to sequence-set scales. 

What we learned using sequence stratigraphy includes: A wide variety of sedimentary structures occur in mudstones that indicate a comparably wide range of transport mechanisms, in many of which the presence of mud alters the fluid and transport properties of the flow. At the parasequence scale, most marine shelfal mudstone strata appear to have accumulated as one of three end-members that can be differentiated quantitatively. These end members can be related to depositional regimes dominated by storm waves, river floods, or tidal currents through characteristic modes of sediment transport and accumulation, as well as variations in benthic-energy and oxygen levels. At the depositional-sequence scale, most marine biogenic-rich mudstones tend to occur in one of three physiographic settings (constructional shelf margin, platform/ramp, continental slope—basin), each of which has a commonly recurring pattern of biogenic enrichment distinctive from the other settings. At the depositional-sequence-set scale, all major shale-gas/shale-oil plays can be grouped into four main families, based on repeated patterns of stratal stacking of depositional-sequence-scale biogenic-rich physiographic settings. 

What we learned about sequence stratigraphy includes: Sequence-stratigraphic criteria (e.g., stratal terminations, geometric relations, stacking patterns) apply across the full range of composition and grain size (> 8 orders of length-scale magnitude). There are a variety of types of surfaces as well as of rocks— and surfaces are indeed much more important than the preserved strata because they record more of geological time (and are commonly easier to recognize in mudstone strata). The same types of surfaces, stratal units, and stacking patterns are seen across all grain sizes and compositions, but their expressions vary as a function of depositional environment.  

Although these observations show that most mudstones accumulate discontinuously, they still preserve detailed records of paleoenvironmental conditions and depositional history, especially in microbially mediated authigenic products. The sequence-stratigraphic approach is particularly useful for organizing all these discontinuities and varying rock properties into a hierarchy of nested scales. Such a hierarchical sequence-stratigraphic framework is essential for integrating the wide range of physical, biogenic, and chemical attributes of mudstones into a comprehensive understanding of Earth history and hydrocarbon systems


Figure 1: Sequence stratigraphic approach reveals characteristic patterns of source-rock distribution and character, even in mudstones. (ORR = organic-matter-rich rocks).


BIOGRAPHY

Kevin M. Bohacs, from Greenwich, Connecticut, received his B.Sc. (Honors) in geology from the University of Connecticut in 1976 and his Sc.D. in experimental sedimentology from M.I.T. in 1981 (where he built and operated the world's largest flume). He joined Exxon Production Research Company in Houston, Texas in 1981, working with Peter Vail, Bob Mitchum, John Van Wagoner, and others on incorporating process-based facies modeling into the development of sequence stratigraphy at the outcrop, core, and well-log scale. Kevin recently retired as Senior Research Scientist from ExxonMobil Upstream Research Company where he led the application of sequence stratigraphy and sedimentology to mudstones from lacustrine to deep-marine environments. He now operates KMBohacs Geoconsulting LLC. His primary focus is to integrate field work, subsurface investigation, and laboratory analyses to inform business decisions. He works closely with exploration groups in evaluating the fine-grained portion of their hydrocarbon systems, teaches field schools in sequence stratigraphy, sedimentology, basin analysis, and field safety leadership, and conducts field work for research and exploration.

Dr. Bohacs has written more than 100 scientific contributions on the stratigraphy and sedimentology of mudstones, hydrocarbon source and reservoir rocks, and continental depositional systems (lakes, fluvial-floodplain systems, paleosols, coals, and paleoichnology, including lake strata on Mars) and conducted field research in more than 42 countries. He has received many best paper citations and awards (most recently, AAPG Honorary Member), is a Fellow of the Geological Society of America, the Geological Society (London), The Explorers Club, and the Royal Geographical Society, and has served as distinguished lecturer for several societies nationally and internationally.