Academic literature on the topic 'Diagenesis models'

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Journal articles on the topic "Diagenesis models"

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Sydnes, Magnhild, Willy Fjeldskaar, Ivar Grunnaleite, Ingrid Fjeldskaar Løtveit, and Rolf Mjelde. "The Influence of Magmatic Intrusions on Diagenetic Processes and Stress Accumulation." Geosciences 9, no. 11 (2019): 477. http://dx.doi.org/10.3390/geosciences9110477.

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Diagenetic changes in sedimentary basins may alter hydrocarbon reservoir quality with respect to porosity and permeability. Basins with magmatic intrusions have specific thermal histories that at time of emplacement and in the aftermath have the ability to enhance diagenetic processes. Through diagenesis the thermal conductivity of rocks may change significantly, and the transformations are able to create hydrocarbon traps. The present numerical study quantified the effect of magmatic intrusions on the transitions of opal A to opal CT to quartz, smectite to illite and quartz diagenesis. We als
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Lanteaume, Cyprien, François Fournier, Matthieu Pellerin, and Jean Borgomano. "Testing geologic assumptions and scenarios in carbonate exploration: Insights from integrated stratigraphic, diagenetic, and seismic forward modeling." Leading Edge 37, no. 9 (2018): 672–80. http://dx.doi.org/10.1190/tle37090672.1.

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Carbonates are considered complex, heterogeneous at all scales, and unfortunately often poorly seismically imaged. We propose a methodology based on forward-modeling approaches to test the validity of common exploration assumptions (e.g., chronostratigraphic value of seismic reflectors) and of geologic interpretations (e.g., stratigraphic correlations and depositional and diagenetic architecture) that are determined from a limited amount of data. The proposed workflow includes four main steps: (1) identification and quantification of the primary controls on carbonate deposition and the predict
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Surdam, Ronald C., Donald B. MacGowan, and Thomas L. Dunn. "Predictive models for sandstone diagenesis." Organic Geochemistry 17, no. 2 (1991): 243–53. http://dx.doi.org/10.1016/0146-6380(91)90081-t.

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Higgs, Karen E., Stuart Munday, Anne Forbes, and Karsten F. Kroeger. "Applications of geochemistry and basin modeling in the diagenetic evaluation of Paleocene sandstones, Kupe Field, New Zealand." Journal of Sedimentary Research 91, no. 9 (2021): 945–68. http://dx.doi.org/10.2110/jsr.2021.020.

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ABSTRACT Paleocene sandstones in the Kupe Field of Taranaki Basin, New Zealand, are subdivided into two diagenetic zones, an upper kaolinite–siderite (K-S) zone and a lower chlorite–smectite (Ch-Sm) zone. Petrographic observations show that the K-S zone has formed from diagenetic alteration of earlier-formed Ch-Sm sandstones, whereby biotite and chlorite–smectite have been altered to form kaolinite and siderite, and plagioclase has reacted to form kaolinite and quartz. These diagenetic zones can be difficult to discriminate from downhole bulk-rock geochemistry, which is largely due to a change
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Adelinet, Mathilde, Jean-François Barthélémy, Elisabeth Bemer, and Youri Hamon. "Effective medium modeling of diagenesis impact on the petroacoustic properties of carbonate rocks." GEOPHYSICS 84, no. 4 (2019): WA43—WA57. http://dx.doi.org/10.1190/geo2018-0559.1.

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Carbonate formations are highly heterogeneous, and the velocity-porosity relationships are controlled by various microstructural parameters, such as the types of pores and their distribution. Because diagenesis is responsible for important changes in the microstructure of carbonate rocks, we have extended the standard effective medium approach to model the impact of diagenesis on the carbonate elastic properties through a step-by-step effective medium modeling. Two different carbonate rocks deposited, respectively, in lacustrine and marine environments are considered in this study. The first k
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Procopio, Noemi, Caley A. Mein, Sefora Starace, Andrea Bonicelli, and Anna Williams. "Bone Diagenesis in Short Timescales: Insights from an Exploratory Proteomic Analysis." Biology 10, no. 6 (2021): 460. http://dx.doi.org/10.3390/biology10060460.

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The evaluation of bone diagenetic phenomena in archaeological timescales has a long history; however, little is known about the origins of the microbes driving bone diagenesis, nor about the extent of bone diagenesis in short timeframes—such as in forensic contexts. Previously, the analysis of non-collagenous proteins (NCPs) through bottom-up proteomics revealed the presence of potential biomarkers useful in estimating the post-mortem interval (PMI). However, there is still a great need for enhancing the understanding of the diagenetic processes taking place in forensic timeframes, and to clar
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Yang, Leilei, Linjiao Yu, Donghua Chen, Keyu Liu, Peng Yang, and Xinwei Li. "Effects of Dolomitization on Porosity during Various Sedimentation-Diagenesis Processes in Carbonate Reservoirs." Minerals 10, no. 6 (2020): 574. http://dx.doi.org/10.3390/min10060574.

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Carbonate reservoirs, especially dolomite reservoirs, contain large reserves of oil and gas. The complex diagenesis is quite challenging to document the dolomite reservoirs formation and evolution mechanism. Porosity development and evolution in dolomite reservoirs primarily reflect the comprehensive effect of mineral dissolution/precipitation during dolomitization. In this study, multicomponent multiphase flow and solute transport simulation was employed to investigate dolomitization in the deep carbonate strata of the Tarim Basin, Northwest China, where active exploration is currently under
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Sorauf, James E. "Biocrystallization models and skeletal structure of Phanerozoic corals." Paleontological Society Papers 1 (October 1996): 159–85. http://dx.doi.org/10.1017/s1089332600000097.

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Modern understanding of skeletal microstructure in fossil corals builds on knowledge of structure and biomineralization in modern corals and diagenesis of carbonate skeletons. It is agreed that the skeleton of living stony corals, the Scleractinia, is made of fibrous aragonite, with growth of biocrystals generally according to rules of crystal growth as observed in inorganic aragonite, but here controlled by organic matrix. Fossil scleractinians all apparently fit the same model of biomineralization seen in living corals, although some early taxa (Triassic) lack septal trabeculae, rod-like fra
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Ma, Shuwei, Dazhong Ren, Lifa Zhou, et al. "Impacts of diagenesis of tight sandstone gas reservoir on reservoir physical properties: A case study, Sulige gas field, Ordos Basin, China." Interpretation 7, no. 3 (2019): T687—T699. http://dx.doi.org/10.1190/int-2018-0173.1.

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Diagenesis is one of the most important factors impacting the performance of many reservoirs and is perhaps the most important factor impacting the performance of tight sandstone reservoirs, such as those of the Sulige gas field in the Ordos Basin of China. However, the relationship between diagenesis and related parameters determining reservoir physical properties remains unclear. Therefore, we have analyzed experimental data from high-pressure mercury intrusion porosimetry, scanning electron microscopy, and thin sections in addition to using a porosity recovery calculation model to investiga
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Chen, Anqing, Shenglin Xu, Shuai Yang, et al. "Ordovician deep dolomite reservoirs in the intracratonic Ordos Basin, China: Depositional model and Diagenetic evolution." Energy Exploration & Exploitation 36, no. 4 (2018): 850–71. http://dx.doi.org/10.1177/0144598718778171.

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Recent natural gas discoveries indicate that non-karstification-dominated reservoirs exist in the intracratonic Ordos Basin. This study examines the sedimentological and geochemical characteristics needed to clarify the depositional model and diagenetic evolution process of this newly discovered reservoir type. The depositional environment of the dolomite reservoir can be characterized as a tidal flat that grew from the Central Paleo-uplift to the eastern depression by cyclic progradation on an epeiric platform. A tidal flat sequence can extend laterally as a progradational wedge in each cycle
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Dissertations / Theses on the topic "Diagenesis models"

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Thornton, David A. "A potential aeolian oil reservoir : the mid Devonian Tandalgoo formation, Canning Basin ; depositional models and diagenesis /." Title page, contents and abstract only, 1990. http://web4.library.adelaide.edu.au/theses/09SM/09smt513.pdf.

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Kalefa, Mohamed. "Diagenesis and Sequence Stratigraphy : Predictive Models for Reservoir Quality Evolution of Fluvial and Glaciogenic and Non-glaciogenic, Paralic Deposits." Doctoral thesis, Uppsala University, Department of Earth Sciences, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-6179.

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<p>Development of a predictive model for the distribution of diagenetic alterations and related evolution of reservoir quality of sandstones was achieved by integrating the knowledge of diagenesis to sequence stratigraphy. This approach allows a better elucidation of the distribution of eogenetic alterations within sequence stratigraphy, because changes in the relative sea level induce changes to: (i) pore water chemistry, (ii) residence time of sediments under certain near-surface geochemical conditions, (iii) variations in the detrital composition, and (iv) amounts and type of organic matter
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Grigg, Nicola Jane, and nicky grigg@csiro au. "Benthic Bulldozers and Pumps: Laboratory and Modelling Studies of Bioturbation and Bioirrigation." The Australian National University. Centre for Resource and Environmental Studies, 2003. http://thesis.anu.edu.au./public/adt-ANU20060228.104425.

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Aquatic sediments are the recipients of a continual rain of organic debris from the water column. The decomposition reactions within the sediment and the rates of material exchange between the sediment and water column are critically moderated by the transport processes within the sediment. The sediment and solute movement induced by burrowing animals – bioturbation and bioirrigation – far exceed abiotic transport processes such as sedimentation burial and molecular diffusion. Thalassinidean shrimp are particularly abundant burrowing animals. Living in high density populations along coastlines
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Wang, Yuexing, and 王越興. "Sediment nutrient flux for a pulsed organic load: mathematical modeling and experimental verfication." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2008. http://hub.hku.hk/bib/B40987826.

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Booler, Jonathan Paul. "Carbonate facies, sequences and associated diagenesis, Upper Cretaceous, Tremp Basin, Spanish Pyrenees." Thesis, Durham University, 1994. http://etheses.dur.ac.uk/5527/.

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This thesis details the results of an integrated study of carbonate platform sedimentology, geometry, evolution and diagenesis within a sequence stratigraphic framework. This study has been based on the Upper Cretaceous carbonates within the Tremp basin of the Spanish Pyrenees, which, through the effects of minor tectonic deformation during the later parts of the Pyrenean orogeny, are exceptionally well exposed and can be studied in the form of a platform to basin cross-section upon a scale that is comparable to that of a seismic section. This study concentrates on the mid-Turonian to Coniacia
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Rabouille, Christophe. "La diagenese precoce : modeles dynamiques et quantitatifs." Paris 7, 1990. http://www.theses.fr/1990PA077161.

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La diagenese precoce des sediments marins profonds contribue au recyclage oceanique des debris biogeniques particulaires. Elle est aussi la premiere etape des transformations que cette matiere subit lors de son enfouissement. Cette etape conduit a des transformations biogeochimiques de la composition des particules qui constituent le sediment et fixe un enregistrement historique des conditions oceaniques. Pour y avoir acces, il est donc necessaire de comprendre et de quantifier les processus de diagenese precoce. Dans cette optique, nous avons developpe des modeles globaux quantitatifs de diag
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JEANDON, CHRISTOPHE. "Reactions modeles de la diagenese des chlorophylles." Université Louis Pasteur (Strasbourg) (1971-2008), 1992. http://www.theses.fr/1992STR13181.

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Les petroporphyrines sont des pigments presents, sous forme de melanges, dans la plupart des sediments contenant de la matiere organique. Ils sont en general les fossiles de chlorophylles. Leur purification chromatographique et l'identification de leurs structures sont souvent difficiles. L'acylation par reaction de friedel-crafts a ete reconsideree en tant qu'outil servant a faciliter la purification de ces melanges complexes et une nouvelle serie de porphyrines diacetylee a ete synthetisee dans ces conditions. Par ailleurs une nouvelle hemisynthese, de deux porphyrines fossiles, la deoxophyl
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ROHRER, ANNICK. "Reactions modeles de la diagenese des porphyrines." Université Louis Pasteur (Strasbourg) (1971-2008), 1995. http://www.theses.fr/1995STR13201.

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Les porphyrines presentes dans la matiere organique sedimentaire (petroporphyrines) sont les fossiles moleculaires de chlorophylles ou d'hemes provenant essentiellement d'algues ou de bacteries. Ces precurseurs biologiques subissent, au cours de leur diagenese, de multiples transformations catalysees par la temperature ou leur environnement chimique (argiles, ions metalliques, soufre et ses derives, etc). Notre travail a consiste a etudier, sur des porphyrines synthetiques, certaines de ces reactions, en particulier les interactions porphyrines-soufre et certains aspects des reactions de metal
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Feleke, Arega Woldemariam. "A diagenetic two-layer eutrophication model for Tolo Harbour, Hong Kong." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2000. http://hub.hku.hk/bib/B31241657.

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Yang, Xin-She. "Mathematical modelling of compaction and diagenesis in sedimentary basins." Thesis, University of Oxford, 1997. http://ora.ox.ac.uk/objects/uuid:0bdc6c43-4534-4f08-97e2-8a33d6b13e61.

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Sedimentary basins form when water-borne sediments in shallow seas are deposited over periods of millions of years. Sediments compact under their own weight, causing the expulsion of pore water. If this expulsion is sufficiently slow, overpressuring can result, a phenomenon which is of concern in oil drilling operations. The competition between pore water expulsion and burial is complicated by a variety of factors, which include diagenesis (clay dewatering), and different modes (elastic or viscous) of rheological deformation via compaction and pressure solution, which may also include hysteres
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Books on the topic "Diagenesis models"

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Boudreau, Bernard P. Diagenetic models and their implementation: Modelling transport and reactions in aquatic sediments. Springer, 1997.

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Diagenetic Models and Their Implementation: Modelling Transport and Reactions in Aquatic Sediments. Springer (originally) but copyrights are held by the author (2003), 1996.

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Boudreau, Bernard P. Diagenetic Models and Their Implementation. Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-60421-8.

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Diagenetic bedding: A model for marl-limestone alternations. Springer-Verlag, 1986.

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Gąsiewicz, Andrzej. Sedymentologia i diageneza wapieni poselenitowych a model genetyczny polskich złóż siarki rodzimej =: Sedimentology and diagenesis of gypsum-ghost limestones and origin of Polish native sulphur deposits. Państwowy Instytut Geologiczny, 2000.

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London, Geological Society of, ed. Mesozoic and Cenozoic carbonate systems of the Mediterranean and the Middle East: Stratigraphic and diagenetic reference models. Geological Society, 2010.

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Márta, Polgári. A Mn geokémiája a feketepala képzödés és a diagenetikus folyamatok tükrében = Manganese geochemistry- reflected by black shale formation and diagenetic processes: Az Úrkúti karbonátos mangánérc képzödési modellje = model of formation of the carbonatic manganese ore of Úrkút. Interbridge Fundation & Karpati Publish House, 1993.

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Diagenetic Bedding: A Model for Marl-Limestone Alternations. Springer-Verlag Berlin and Heidelberg GmbH & Co. KG, 1986.

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Hoffmann, Heidi. Depositional and diagenetic model for the Middle Devonian Denay Limestone, northern Antelope Range, Eureka County, Nevada. 1989.

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Book chapters on the topic "Diagenesis models"

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Maliva, Robert G. "Carbonate Facies Models and Diagenesis." In Springer Hydrogeology. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-32137-0_4.

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Van Cappellen, Philippe, Jean-François Gaillard, and Christophe Rabouille. "Biogeochemical Transformations in Sediments: Kinetic Models of Early Diagenesis." In Interactions of C, N, P and S Biogeochemical Cycles and Global Change. Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-76064-8_17.

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Smith, Craig R. "Factors Controlling Bioturbation in Deep-Sea Sediments and Their Relation to Models of Carbon Diagenesis." In Deep-Sea Food Chains and the Global Carbon Cycle. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-2452-2_23.

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Perrin, Christine. "Diagenesis." In Encyclopedia of Modern Coral Reefs. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2639-2_12.

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Aissaoui, D. M., D. Buigues, and B. H. Purser. "Model of Reef Diagenesis: Mururoa Atoll, French Polynesia." In Reef Diagenesis. Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-642-82812-6_3.

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Boudreau, Bernard P. "Model Construction." In Diagenetic Models and Their Implementation. Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-60421-8_3.

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Boudreau, Bernard P. "The Philosophy of Diagenetic Modelling." In Diagenetic Models and Their Implementation. Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-60421-8_1.

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Boudreau, Bernard P. "Appendix: How to Obtain Fortran Codes." In Diagenetic Models and Their Implementation. Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-60421-8_10.

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Boudreau, Bernard P. "References." In Diagenetic Models and Their Implementation. Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-60421-8_11.

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Boudreau, Bernard P. "Common and Important Symbols." In Diagenetic Models and Their Implementation. Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-60421-8_12.

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Conference papers on the topic "Diagenesis models"

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Al Subait, Ali, Kadhem Al-Nasser, Najm Alqahtani, and Ammar Agnia. "Enhanced Reservoir Characterization of Complex Carbonates by Integrating Diagenesis with Petrophysical Properties." In SPE Annual Technical Conference and Exhibition. SPE, 2022. http://dx.doi.org/10.2118/210457-ms.

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Abstract Carbonate reservoir characterization is often challenging due to variable mineralogy, pore-geometry, texture, and diagenetic processes that modified the rock fabric and its petrophysical properties affecting rock typing, reservoir-potential evaluation, and deliverability prediction. This work implements a multidisciplinary petrophysical discrimination scheme that draws upon the diagenetic history of the rock to resolve such characterization challenges and optimize field development practices. This study integrates sequence stratigraphy, core description, petrography, diagenetic analys
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Vorobiev, S., M. Altunbay, and K. B Salleh. "Tackling Diagenesis: Rock Physics Models Applications into Advanced Petrophysics." In EAGE/FESM Joint Regional Conference Petrophysics Meets Geoscience. EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20132102.

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"Comparison of organic matter oxidation approaches in sediment diagenesis models." In 19th International Congress on Modelling and Simulation. Modelling and Simulation Society of Australia and New Zealand (MSSANZ), Inc., 2011. http://dx.doi.org/10.36334/modsim.2011.i7.paraska.

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Burdige, David, Tomoko Komada, and Hussain Abdulla. "Linking Dissolved Organic Matter Composition Data to Reaction-Transport Models of Sediment Diagenesis." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.283.

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Gordin, Yair, Thomas Bradley, Yoav O. Rosenberg, Anat Canning, Yossef H. Hatzor, and Harold J. Vinegar. "Relating Acoustic Anisotropy to Kerogen Content in Unconventional Formations - A Case Study in A Kerogen-Rich Unconventional Carbonate." In SPE Annual Technical Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/205912-ms.

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Abstract The mechanical and petrophysical behavior of organic-rich carbonates (ORC) is affected significantly by burial diagenesis and the thermal maturation of their organic matter. Therefore, establishing Rock Physics (RP) relations and appropriate models can be valuable in delineating the spatial distribution of key rock properties such as the total organic carbon (TOC), porosity, water saturation, and thermal maturity in the petroleum system. These key rock properties are of most importance to evaluate during hydrocarbon exploration and production operations when establishing a detailed su
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Ait-Ettajer, Taoufik, Laurent Fontanelli, and Lakshmikantha Mookanahallipatna. "Improving Drilling Success by Integrating Sedimentology and Diagenesis models: Case Study from South America." In Offshore Technology Conference. Offshore Technology Conference, 2015. http://dx.doi.org/10.4043/25951-ms.

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Nadeau, P. H., P. A. Bjørkum, and O. Walderhaug. "Thermo-Chemical Models for Silicate Diagenesis, Overpressure and Hydrocarbon Resource Distributions - The Gulf of Mexico Evidence." In 63rd EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2001. http://dx.doi.org/10.3997/2214-4609-pdb.15.o-34.

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Al-Nasser, Kadhem, and Mahmoud Alnazghah. "Novel Modeling Approach of Carbonate Reservoirs by Integrating Geological Facies, Diagenesis, and Wireline Logs for Field Development with Insights into Low Resistivity Pay." In International Petroleum Technology Conference. IPTC, 2022. http://dx.doi.org/10.2523/iptc-21870-ms.

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Abstract Characterizing carbonate reservoirs is challenging due to their inherent complex nature, while diagenetic overprint causes an added layer of complexity. Diagenesis may enhance or deteriorate reservoir properties resulting in a wide range of pertinent rock types. The studied reservoirs consist of several shallowing upward cycles, which are capped by tidal flats lithofacies and evaporites, governing the spatial and temporal distribution of the reservoir units. In this work, we have used existing data to link sedimentology, stratigraphy, diagenesis, and wireline logs to build a full-fiel
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Massonnat, Gérard Joseph, Charles Danquigny, Emmanuelle Leonforte, Lucie Dal Soglio, Mickael Barbier, and Jean-Louis Lesueur. "A Multi-Process Reservoir Modelling Workflow as the Key for Unlocking Reservoir Prediction in Carbonates. Application to a Sector Model from the Albion R&D Project." In Abu Dhabi International Petroleum Exhibition & Conference. SPE, 2021. http://dx.doi.org/10.2118/207556-ms.

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Abstract In carbonate reservoirs, because of the diversity of geological processes involved in the reservoir construction, the extrapolation of properties directly from well data to reservoir model gridblocks may lead to poorly predictive reservoir properties and then production forecasts. This paper proposes a modelling workflow in which new tools from disruptive technologies are associated in order to produce reservoir models consistently with reservoir geological construction. The workflow combines the simulation of the depositional facies and their transformation after diagenesis overprint
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Riaño Caraza, Juan M., Fernando S. Flores Avila, Iván Faría Rojas, and Luis E. Brito Rodríguez. "Development of a Performance Assessment Model (PAM) for High Complexity Non-Conventional Reservoirs." In ASME 2012 31st International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/omae2012-84183.

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Chicontepec is one of the areas with the largest volume of original oil in place in Mexico; however, after more than 30 years of operation, its development has been very limited due to the high geological complexity and low rock quality of their reservoirs. The reservoirs are found in layered sequences of sediments deposited in turbiditic environments which have suffered different degrees of diagenesis, there is a great level of vertical heterogeneity and a very limited level of lateral continuity. The permeability of the reservoir area is in the range of 0.1 to 5 md, depending on the location
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Reports on the topic "Diagenesis models"

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Lasaga, A. C., and D. M. Rye. Reactive fluid flow models and applications to diagenesis, mineral deposits and crustal rocks. Office of Scientific and Technical Information (OSTI), 1992. http://dx.doi.org/10.2172/6973243.

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Lasaga, A. C., and D. M. Rye. Reactive fluid flow models and applications to diagenesis, mineral deposits and crustal rocks. Office of Scientific and Technical Information (OSTI), 1993. http://dx.doi.org/10.2172/10173566.

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Lasaga, A. C., and D. M. Rye. Reactive fluid flow models and applications to diagenesis, mineral deposits and crustal rocks. Progress report. Office of Scientific and Technical Information (OSTI), 1992. http://dx.doi.org/10.2172/10183433.

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Kingston, A. W., O. H. Ardakani, and R A Stern. Tracing the subsurface sulfur cycle using isotopic and elemental fingerprinting: from the micro to the macro scale. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329789.

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Hydrogen sulfide (H2S) is a toxic and corrosive gas that commonly occurs in deeply buried sedimentary systems. Understanding its distribution is paramount to creating safe and effective models of H2S occurrence aiding in the identification of high-risk areas. Characterizing subsurface sulfur sources and H2S formation pathways would enhance these models leading to more accurate predictions of potential high H2S regions. However, gaps remain in our understanding of the dominant formation processes and migration pathways of key ingredients for H2S production in the Lower Triassic Montney Formatio
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Johnson, Billy E., and Zhonglong Zhang. Testing and Validation Studies of the NSMII-Benthic Sediment Diagenesis Module. Defense Technical Information Center, 2016. http://dx.doi.org/10.21236/ad1012495.

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Simandl, G. J., R. J. D'Souza, S. Paradis, and J. Spence. Rare-earth element content of carbonate minerals in sediment-hosted Pb-Zn deposits, southern Canadian Rocky Mountains. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328001.

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Abstract:
Paleozoic platform carbonate rocks of the Rocky Mountains host Mississippi Valley-type (MVT), magnesite, barite, and REE-barite-fluorite deposits. Farther west, platform carbonate rocks of the Kootenay Arc host MVT and fracture-controlled replacement (FCR) deposits. This is the first systematic LA-ICP-MS study of carbonates in MVT and FCR deposits. We investigated seven MVT deposits in the Rocky Mountains, and five MVT deposits in the Kootenay Arc. None of the post-Archean Australian shale (PAAS)-normalized REE profiles show light REE (LREE) depletion and strong negative Ce anomalies character
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Chidsey, Thomas C., David E. Eby, Michael D. Vanden Berg, and Douglas A. Sprinkel. Microbial Carbonate Reservoirs and Analogs from Utah. Utah Geological Survey, 2021. http://dx.doi.org/10.34191/ss-168.

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Abstract:
Multiple oil discoveries reveal the global scale and economic importance of a distinctive reservoir type composed of possible microbial lacustrine carbonates like the Lower Cretaceous pre-salt reservoirs in deepwater offshore Brazil and Angola. Marine microbialite reservoirs are also important in the Neoproterozoic to lowest Cambrian starta of the South Oman Salt Basin as well as large Paleozoic deposits including those in the Caspian Basin of Kazakhstan (e.g., Tengiz field), and the Cedar Creek Anticline fields and Ordovician Red River “B” horizontal play of the Williston Basin in Montana and
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