Abstract:Quantitative data on geobodies are crucial for reservoir modelling. Although abundant quantitative data are available in the literature for siliciclastic depositional systems, equivalent data for carbonate systems are scarce. In this paper we introduce a new approach to the management of quantitative data on carbonate geobodies which is based on a hierarchical classification scheme. The classes to which a carbonate geobody are assigned are: (1) depo-time (i.e. geological age); (2) depo-system (i.e. type of car… Show more
“…However, the initial depositional texture also profoundly influences the stratabound dolostone geobodies; therefore, the depositional classification of geobodies of Jung and Aigner (2012) can be applied to this type of diagenetic geobodies (stratabound geobodies at Wadi Mistal would correspond in this classification to a Jurassic ramp system in the protected platform zone and with a "sheet" shape, see Table 1A). …”
Section: Control On Dolomite Geobody Dimensions Diagenetic Geobody Cmentioning
confidence: 99%
“…Several studies such as Harris et al (2011) focused on quantifying dimensions of carbonate sand bodies and their spatial patterns. Recent efforts led to a hierarchical classification scheme of carbonate geobodies and a set of rules to characterize their dimension, shape, orientation and spatial distribution as a basis for reservoir modeling (Jung and Aigner, 2012). Components of this classification scheme includes geological time, system, zone, shape, element and facies of deposition (Jung and Aigner, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Recent efforts led to a hierarchical classification scheme of carbonate geobodies and a set of rules to characterize their dimension, shape, orientation and spatial distribution as a basis for reservoir modeling (Jung and Aigner, 2012). Components of this classification scheme includes geological time, system, zone, shape, element and facies of deposition (Jung and Aigner, 2012). Aside from shape, all of the components in the Jung and Aigner (2012) classification are related to sedimentology and depositional environment; diagenetic geobodies are not taken into consideration (Table 1A).…”
Section: Introductionmentioning
confidence: 99%
“…Components of this classification scheme includes geological time, system, zone, shape, element and facies of deposition (Jung and Aigner, 2012). Aside from shape, all of the components in the Jung and Aigner (2012) classification are related to sedimentology and depositional environment; diagenetic geobodies are not taken into consideration (Table 1A).…”
Section: Introductionmentioning
confidence: 99%
“…We then combine this dataset with a structural analysis, and compare the above dataset to the geobodies dimensions, shape and distribution in order to assess how processes impact on geobody dimensions and geometries. This leads us to propose a simple modification to the Jung and Aigner (2012) classification for geobodies for the purpose of reservoir modeling.…”
Understanding the distribution and geometry of reservoir geobodies is crucial for netto-gross estimates and to model subsurface flow. This paper focuses on the process of dolomitization and resulting geometry of diagenetic geobodies in an outcrop of Jurassic host rocks from northern Oman. Field and petrographic data show that a first phase of stratabound dolomite is crosscut by a second phase of fault-related dolomite. The stratabound dolomite geobodies are laterally continuous for at least several hundreds of meters (~1000 ft) and probably regionally and are half a meter (1.6 ft) thick. Based on petrography and geochemistry, a process of seepage reflux of mesosaline or hypersaline fluids during the early stages of burial diagenesis is proposed for the formation of the stratabound dolomite. In contrast, the fault-related dolomite geobodies are trending along a fault that can be followed for at least 100
Running head:Linking process, dimension, texture and geochemistry in dolomite geobodies
“…However, the initial depositional texture also profoundly influences the stratabound dolostone geobodies; therefore, the depositional classification of geobodies of Jung and Aigner (2012) can be applied to this type of diagenetic geobodies (stratabound geobodies at Wadi Mistal would correspond in this classification to a Jurassic ramp system in the protected platform zone and with a "sheet" shape, see Table 1A). …”
Section: Control On Dolomite Geobody Dimensions Diagenetic Geobody Cmentioning
confidence: 99%
“…Several studies such as Harris et al (2011) focused on quantifying dimensions of carbonate sand bodies and their spatial patterns. Recent efforts led to a hierarchical classification scheme of carbonate geobodies and a set of rules to characterize their dimension, shape, orientation and spatial distribution as a basis for reservoir modeling (Jung and Aigner, 2012). Components of this classification scheme includes geological time, system, zone, shape, element and facies of deposition (Jung and Aigner, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Recent efforts led to a hierarchical classification scheme of carbonate geobodies and a set of rules to characterize their dimension, shape, orientation and spatial distribution as a basis for reservoir modeling (Jung and Aigner, 2012). Components of this classification scheme includes geological time, system, zone, shape, element and facies of deposition (Jung and Aigner, 2012). Aside from shape, all of the components in the Jung and Aigner (2012) classification are related to sedimentology and depositional environment; diagenetic geobodies are not taken into consideration (Table 1A).…”
Section: Introductionmentioning
confidence: 99%
“…Components of this classification scheme includes geological time, system, zone, shape, element and facies of deposition (Jung and Aigner, 2012). Aside from shape, all of the components in the Jung and Aigner (2012) classification are related to sedimentology and depositional environment; diagenetic geobodies are not taken into consideration (Table 1A).…”
Section: Introductionmentioning
confidence: 99%
“…We then combine this dataset with a structural analysis, and compare the above dataset to the geobodies dimensions, shape and distribution in order to assess how processes impact on geobody dimensions and geometries. This leads us to propose a simple modification to the Jung and Aigner (2012) classification for geobodies for the purpose of reservoir modeling.…”
Understanding the distribution and geometry of reservoir geobodies is crucial for netto-gross estimates and to model subsurface flow. This paper focuses on the process of dolomitization and resulting geometry of diagenetic geobodies in an outcrop of Jurassic host rocks from northern Oman. Field and petrographic data show that a first phase of stratabound dolomite is crosscut by a second phase of fault-related dolomite. The stratabound dolomite geobodies are laterally continuous for at least several hundreds of meters (~1000 ft) and probably regionally and are half a meter (1.6 ft) thick. Based on petrography and geochemistry, a process of seepage reflux of mesosaline or hypersaline fluids during the early stages of burial diagenesis is proposed for the formation of the stratabound dolomite. In contrast, the fault-related dolomite geobodies are trending along a fault that can be followed for at least 100
Running head:Linking process, dimension, texture and geochemistry in dolomite geobodies
In inverse problems, investigating uncertainty in the posterior distribution of model parameters is as important as matching data. In recent years, most efforts have focused on techniques to sample the posterior distribution with reasonable computational costs. Within a Bayesian context, this posterior depends on the prior distribution. However, most of the studies ignore modeling the prior with realistic geological uncertainty. In this paper, we propose a workflow inspired by a Popper-Bayes philosophy that data should first be used to falsify models, then only be considered for matching. We propose a workflow consisting of three steps: (1) in defining the prior, we interpret multiple alternative geological scenarios from literature (architecture of facies) and site-specific data (proportions of facies). Prior spatial uncertainty is modeled using multiplepoint geostatistics, where each scenario is defined using a training image. (2) We validate these prior geological scenarios by simulating electrical resistivity tomography (ERT) data on realizations of each scenario and comparing them to field ERT in a lower dimensional space. In this second step, the idea is to probabilistically falsify scenarios with ERT, meaning that scenarios which are incompatible receive an updated probability of zero while compatible scenarios receive a nonzero updated belief. (3) We constrain the hydrogeological model with hydraulic head and ERT using a stochastic search method. The workflow is applied to a synthetic and a field case studies in an alluvial aquifer. This study highlights the importance of considering and estimating prior uncertainty (without data) through a process of probabilistic falsification.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.