Zobrazeno 1 - 10
of 47
pro vyhledávání: '"Randall L. Mackie"'
Publikováno v:
GEOPHYSICS. 86:E157-E170
In 2010, an exploration well was drilled at the Lona prospect in the Orphan Basin, Canada, whose location was based primarily on a structural high at the base of a Cretaceous unconformity. Additionally, a 3D inversion of controlled-source electromagn
Autor:
Roger V. Miller, Randall L. Mackie, Ahmad Shahir Saleh, Max A. Meju, Federico Miorelli, Carsten Scholl
Publikováno v:
Interpretation. 8:SS1-SS13
Geologic interpretation of resistivity models from marine controlled-source electromagnetic (CSEM) and magnetotelluric (MT) data for hydrocarbon exploration and reservoir monitoring can be problematic due to structural complexity and low-resistivity
Publikováno v:
ASEG Extended Abstracts. 2019:1-4
We have quantified the use of finite electric dipole lengths from the point measurement assumptions typical in 3D MT inversion modeling. Electric fields are measured across dipoles of typically 50 ...
Publikováno v:
GEOPHYSICS. 84:E387-E402
Geologic interpretation of 3D anisotropic resistivity models from conventional marine controlled-source electromagnetic (CSEM) data inversion faces difficulties in low-resistivity contrast sediments and structurally complex environments that typify t
Autor:
Wolfgang Soyer, Randall L. Mackie
Publikováno v:
ASEG Extended Abstracts. 2018:1-7
Ground Magnetotelluric (MT) data acquired today are typically broadband, covering 0.001 to >1000 Hz with inter-site spacing typically at 500 to 1000 m. Airborne Z-axis tipper data (ZTEM) are sampled at higher spatial density but usually band-limited
Publikováno v:
SEG Technical Program Expanded Abstracts 2020.
Publikováno v:
SEG Technical Program Expanded Abstracts 2020.
Publikováno v:
NSG2020 3rd Conference on Geophysics for Mineral Exploration and Mining.
Summary Controlled source, grounded electrode EM surveys have a long and successful history in mineral exploration geophysics, where the most commonly deployed configuration is CSAMT, which uses single, fixed, kilometre-long transmitter dipoles (e.g.
Publikováno v:
1st Geoscience & Engineering in Energy Transition Conference.
Summary Following from our recent work on joint inversion of MT, gravity, and MEQ data from the Darajat field ( Soyer et al, 2018 ), here we illustrate the pros and cons of quantitative integration of MT and gravity data through 3D joint inversion mo
Publikováno v:
EAGE 2020 Annual Conference & Exhibition Online.
Summary We have implemented 3D faults as discontinuity surfaces, of finite extent, in the regularization step of our non-linear inversion engine (RLM-3D), for both single domain and cross-gradient joint inversion cases, and applied this for geotherma