Zobrazeno 1 - 10
of 100
pro vyhledávání: '"Tom Manzocchi"'
Autor:
Md Saiful Islam, Tom Manzocchi
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
Abstract Faults are generally represented in conventional upscaled models as 2D planar surfaces with transmissibility multipliers used to represent single-phase fault properties. However, faults are structurally complex 3D zones in which both single-
Externí odkaz:
https://doaj.org/article/76da63cff14f4366a617aa67311cf7ba
Autor:
Tom Manzocchi, Deirdre A. Walsh
Publikováno v:
Mathematical Geosciences. 55:461-496
Equations describing facies proportions and amalgamation ratios are derived for randomly placed objects belonging to two or three foreground facies embedded in a background facies, as a function of the volume fractions and object thicknesses of indep
Publikováno v:
Mathematical Geosciences.
Simple object- or pixel-based facies models use facies proportions as the constraining input parameter to be honored in the output model. The resultant interconnectivity of the facies bodies is an unconstrained output property of the modelling, and i
Publikováno v:
Springer Proceedings in Earth and Environmental Sciences ISBN: 9783031198441
Pixel-based multiple-point statistical (MPS) modelling is an appealing geostatistical modelling technique as it easily honours well data and allows use of geologically-derived training images to reproduce the desired heterogeneity. A variety of diffe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7cb076b1c786a2d6c78521f13acd250c
https://doi.org/10.1007/978-3-031-19845-8_10
https://doi.org/10.1007/978-3-031-19845-8_10
Publikováno v:
Springer Proceedings in Earth and Environmental Sciences ISBN: 9783031198441
In object- or pixel-based modelling, facies connectivity is tied to facies proportion as an inevitable consequence of the modelling process. However, natural geological systems (and rule-based models) have a wider range of connectivity behaviour and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d85d6f79450d0cc917259c2ae9404a3a
https://doi.org/10.1007/978-3-031-19845-8_8
https://doi.org/10.1007/978-3-031-19845-8_8
Publikováno v:
Natural Resources Research. 30:2561-2573
Most petroleum reservoirs contain faults, and a key methodological challenge in full-field reservoir modeling is to include the effects of 3D sub-seismic fault zone structure within the 2D fault surfaces represented in commercially available simulato
Autor:
Saiful Islam, Tom Manzocchi
Publikováno v:
Scientific Reports
Scientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
Scientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
Faults are generally represented in conventional upscaled models as 2D planar surfaces with transmissibility multipliers used to represent single-phase fault properties. However, faults are structurally complex 3D zones in which both single-phase and
Autor:
John Conneally, Tom Manzocchi, Giovanni Camanni, John J. Walsh, Vincent Roche, Muhammad Mudasar Saqab, Efstratios Delogkos, Conrad Childs
Normal faults are often complex three-dimensional structures comprising multiple sub-parallel segments separated by intact or breached relay zones. In this study we outline geometrical characterisations capturing this 3D complexity and providing a se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da7cdaee60b3e1ce2d3503647848bc9a
https://doi.org/10.5194/egusphere-egu21-15228
https://doi.org/10.5194/egusphere-egu21-15228
Autor:
Tom Manzocchi
Faults can control the large-scale properties of rock volumes through their behaviour as flow conduits and/or barriers or by localising geomechanical effects. Hence, often the fidelity of a numerical model of faulted site relies on the accuracy with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::679d0e945520e7a52eed0f2b2ca88947
https://doi.org/10.5194/egusphere-egu21-7348
https://doi.org/10.5194/egusphere-egu21-7348
The state of stress in the shallow crust of the Hikurangi Subduction Margin hangingwall, New Zealand
Knowledge of in situ stress fields is critical for a better understanding of deformation, faulting regime, and earthquake processes in seismically active margins such as the Hikurangi Subduction Margin (HSM), North Island, New Zealand. In this study,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8e509b6d714c01f391ddb099ba2d577
https://doi.org/10.5194/egusphere-egu21-10217
https://doi.org/10.5194/egusphere-egu21-10217