Abstract: Joint PP and PS AVO Inversion Based on Zeopprtiz Equations; #90171 (2013)

Tiansheng Chen and Xiucheng Wei

Search and Discovery.com

... are nonlinear functions with respect to the six elastic parameters, such as α1 , α 2 , β1 , β 2 , ρ1 , ρ 2 , The ultimate goal of an AVO inversion method...

Abstract: Joint PP and PS AVO Inversion Based on Zeopprtiz Equations; #90171 (2013)

Tiansheng Chen and Xiucheng Wei

Search and Discovery.com

... are nonlinear functions with respect to the six elastic parameters, such as α1 , α 2 , β1 , β 2 , ρ1 , ρ 2 , The ultimate goal of an AVO inversion method...

Technology Explained: From Arrhenius to CO2 Storage … Part XVI: A Greenhouse Model for Stratospheric Cooling … 2

Lasse Amundsen, Martin Landrø

GEO ExPro Magazine

... the window-grey mo by the The source β Goessling andthe factor 1-δ compared to the grey model case. The differential equations that govern case...

Latest Quaternary Baram Prodelta, Northwestern Borneo

Richard N. Hiscott

Special Publications of SEPM

... youngest to oldest, α, β, δ, γ, and ε). These lobes are located directly seaward of the FIG. 1.—A) Regional geography of southeast Asia, with country names...

Character of the Relationship Between Permeability and the Total and Dynamic Porosity of Rocks

M. Sh. Pernikov

Petroleum Geology: A Digest of Russian Literature

... pores, the coefficient of permeability (kper) can be represented by the formula: (1) k per = Am n β where A is a coefficient...

Geochemical Characterization, Depositional Environment, and Controlling Factors of B-Carotene - A Case Study of Jimsar Depression, Junggar Basin of China, #11002 (2017).

Xiujian Ding, Ming Zha, Xulong Wang, Yang Su, Changhai Gao, Jiangxiu Qu, Ren Lai

Search and Discovery.com

... Environment, and Controlling Factors of β-Carotene - A Case Study of Jimsar Depression, Junggar Basin of China* Xiujian Ding1, Ming Zha1, Xulong Wang2...

ABSTRACT: DEPENDENCE OF ABNORMAL PRESSURES FROM TENSION IN THE ROCK; #90011 (2002)

A. A. Orlov, V. G. Omelchenko, I. R. Mykhailiv, A. M. Trubenko

Search and Discovery.com

.... These values can be taken into account with the help elasticity coefficient Then ∆P=∆σ x,y β, there from ∆ σ x,y = ∆Ρ . β AAPG Search...

Abstract: The Crystal Chemistry of Manitobaite, (Na16 ) Mn2+25 Al8 (PO4)30, ANew Phosphate Mineral of the Alluaudite-Group (sensu late) from Cross Lake, Manitoba, Canada; #90172 (2014)

Kim Tait, Mark A. Cooper, Yassir Abdu, Frank C. Hawthorne, T. Scott Ercit

Search and Discovery.com

... and calculated densities are 3.621(6) and 3.628 gcm-3, respectively. Manitobaite is biaxial negative with α 1.682, β 1.691, γ 1.697, (all ± 0.001), with X...

Diffusion of Carbon Dioxide Across Rock Salt

P. L. Antonov П. Л. Антонов, G. A. Gladysheva Г. А. Гладышева, V. P. Kozlov В. П. Козлов

Petroleum Geology: A Digest of Russian Literature

... in Fig. 1 and is determined by the formula: Q = π r 2 β C o l ( D t l 2 - 1 6 + 2 π 2 × × ∑ 1 n - 1 n...

From Arrhenius to CO2 Storage: Part XIII: The Temperature Profile in a Grey Atmosphere

Lasse Amundsen, Martin Landrø

GEO ExPro Magazine

... have the same dependence on height, Goessling and Bathiany (2016) suggest introducing a new β is constant. This property of β makes equations 2a...

Hydraulic Fracture Propagation in Fractured Media, #50315 (2010)

Marc Thiercelin, Dimitry Chuprakov, Eduard Siebrits, Robert Jeffrey, Xi Zhang

Search and Discovery.com

... Model: Governing Equations Elastic deformation  N r ∫ [G ( x , s , α , β ) w( s ) + G ( x , s , α , β )v ( s )]ds 11 12 r =1 0 σ n ( x, t ) − σ 1...

DiffSim: Denoising diffusion probabilistic models for generative facies geomodeling

Minghui Xu, Suihong Song, Tapan Mukerji

International Meeting for Applied Geoscience and Energy (IMAGE)

..., 𝑞(𝑥% |𝑥%'( ) = 𝑁,𝑥% ; .1 − β% 𝑥%'( , β% 𝑰4, 𝑡 ∈ {1, . . . , 𝑇}, where 𝑞(𝑥% |𝑥%'( ) follows the Gaussian distribution, β% represents the variance of the added...

ABSTRACT: Application of the Kissinger equation to the problem of evaluating reaction kinetics using T[sub]max[/sub] and formation temperature data from the Tyler Formation (Pennsylvanian) of North Dakota., by Stephen Nordeng; #90156 (2012)

Search and Discovery.com

Assessment of Micro-Fracture Density using Combined Interpretation of NMR Relaxometry and Electromagnetic Logs

Lu Chi, Marcus, Elliot, Zoya Heidari, Mark Everett

Unconventional Resources Technology Conference (URTEC)

... walk. We represent this by applying a spatially uniform roughness parameter, β (Bray, 2013). This parameter represents the waiting time distribution...

Regularization by robust denoising for iterative simultaneous source separation

Breno Bahia, Mauricio D. Sacchi

International Meeting for Applied Geoscience and Energy (IMAGE)

..., let β = NN·Ns define the blending factor, tb and µ > 0 the regularization parameter. The regularization term in equation 1 applies the denoiser...

Distribution and Composition of Disseminated Organic Matter in Sediments of the Neogene, Paleogene, and Cretaceous of the Trans-Carpathian Downwarp

G. M. Karpenko, Ye. F. Shevchenko

Petroleum Geology: A Digest of Russian Literature

.... Figure 1. Variation in bitumen content (β) of organic matter in rocks of the Neogene, Paleogene, and Cretaceous of the Trans-Carpathian downwarp...

Abstract: Prediction of blast induced vibration at Lafarge Quarry in Kanthan, Ipoh, Perak

Mohd Hazizan Mohd Hashim, Khairul Shazwan Pelawang, Shaib Abdulazeez Shehu

Geological Society of Malaysia (GSM)

..., K and β values as 1140 and -1.6 respectively. However, these values are adaptation from Australian Standards (AS 2187.2 -1993), where Standard...

Rigorous and Innovative Risk Quantification for Basin Modeling

A. Medina, J-M Laigle, M. Pontet

Asociación Colombiana de Geólogos y Geofisicos del Petróleo (ACGGP)

... (modelling). In this case the model to be computed is as follow: Y = β 0 + β1 A + β 2 B + β 3C + β 4 D + β5 E + β 6 F + β12 AB + β13 AC + β14 AD + β15 AE...

Determination of Oil-Water Saturation and Position of the Water-Oil Contact in Carbonate Reservoirs of Fields of the Kuybyshev Region by Radiometric Methods

L. Z. Tslav, V. V. Laptev

Petroleum Geology: A Digest of Russian Literature

... for standardized parameters: J ́ x - J ́ 1 J ́ 2 - J ́ 1 = β ́ and J ́ ́ x - J ́ ́ 1 J ́ ́ 2 - J ́ ́ 1 = β ́ ́ . It is neces...

Improving Infill Development Decision Making with Interval Estimation; #110062 (2008)

J. Marcus Jobe and T. Hutch Jobe

Search and Discovery.com

... + σ 2 / 2) Weibull Distribution scale parameter α = 1 selected shape parameter β values β β ⎛x⎞ f ( x) = ( β ) x β −1 exp[−⎜ ⎟ ], x > 0 α ⎝α ⎠ Mean...

Geochemical Allocation of Commingled Oil Production and/or Commingled Gas Production from 2-6 Pay Zones, #90110 (2010)

Mark A. McCaffrey, David K. Baskin, Brooks A. Patterson, Jeremy E. Dahl, Kate S. Weissenburger

Search and Discovery.com

... relationship of the form: Y = β1X1 + β2X2 + ... βmXm. Production allocation is the process of determining the values of β. However, in reality...

Origin of heavy shale oil in saline lacustrine basins: Insights from the Permian Lucaogou Formation, Junggar Basin

Yuce Wang, Jian Cao, Keyu Tao, Chenjia Zhang, Baoli Xiang, Erting Li, Shuang Yu, and Changchun Pan

AAPG Bulletin

... and environment) caused by different depositional paleoenvironments between the upper and lower sections of the formation. The higher β-carotane...

A finite-element method to compute the seismic response in non-isothermal poroelastic media

Juan E. Santos, Gabriela B. Savioli, Jos M. Carcione, Jing Ba

International Meeting for Applied Geoscience and Energy (IMAGE)

... relations σi j (u, θ ) = p f (u, θ ) = 2µ εi j (us ) +δi j (λu ∇ · us + B∇ · u f − β θ ), s f −B ∇ · u − M∇ · u + β f θ . (1) (2) Biot’s dynamical...

From Arrhenius to CO2 Storage: Part VII: Arrhenius' Greenhouse Rule for CO2

Lasse Amundsen, Martin Landrø

GEO ExPro Magazine

... where the surface temperature has increased by ∆T. Equation (1) in Part VI defines the new temperature as T(β + Δβ). For a sufficiently small...

ABSTRACT: A GEOCHEMICAL/MATHEMATICAL APPROACH TO VITRINITE REFLECTANCE

J. W. Smith, J. R. Smith

The Society for Organic Petrology (TSOP)

... regression analysis: Ro = α βC + λH + (1) Where: -2 -2 -2 α = – (5.035 ± 0.513) x10 , β = (8.04 ± 0.50) x10 and λ = – (18 ± 2) x10 . The values...