Results 201 to 210 of about 11,537 (242)
Lamination-Controlled Lithofacies Differentiation and Shale Oil Enrichment: A Case Study of the Qingshankou Formation, Songliao Basin. [PDF]
Yao Q +9 more
europepmc +1 more source
Comprehensive risk mapping and management of rainfall-induced slope failures in urbanizing subtropical regions. [PDF]
Yang F, Hasan M.
europepmc +1 more source
A conditioning factor selection framework considering sample heterogeneity in debris flow susceptibility mapping. [PDF]
Gao R, Wang A, Wu D.
europepmc +1 more source
11th Urals Lithological Meeting and 2nd Youth School on Lithology
A. V. Maslov, V. P. Alekseev
openaire +2 more sources
Some of the next articles are maybe not open access.
Related searches:
Related searches:
SEG Technical Program Expanded Abstracts 1983, 1983
Seismic data constitute a noise-contaminated bandlimited representation of lithologic information. Therefore, attempts to recover lithologic information, such as velocity and density of thin layers, from seismic data cannot give a unique or verifiably correct result.
Valery Gelfand, Ken Larner
openaire +1 more source
Seismic data constitute a noise-contaminated bandlimited representation of lithologic information. Therefore, attempts to recover lithologic information, such as velocity and density of thin layers, from seismic data cannot give a unique or verifiably correct result.
Valery Gelfand, Ken Larner
openaire +1 more source
2016
The Macraes deposit is developed in the regional scale Hyde-Macraes Shear Zone, which was mineralised under lower greenschist facies conditions. The shear zone is >500 m thick and structurally overlies upper greenschist facies rocks. Host schists have two end-member rock types: micaceous schist and feldspathic schist, and these are interlayered at all ...
Dave Craw, Doug MacKenzie
openaire +1 more source
The Macraes deposit is developed in the regional scale Hyde-Macraes Shear Zone, which was mineralised under lower greenschist facies conditions. The shear zone is >500 m thick and structurally overlies upper greenschist facies rocks. Host schists have two end-member rock types: micaceous schist and feldspathic schist, and these are interlayered at all ...
Dave Craw, Doug MacKenzie
openaire +1 more source
2000
Abstract Lithology and fluid information can be extracted from seismic data of deepwater clastics if their relative contribution to the signal is understood. Brushy Canyon Formation outcrop seismic models are constructed for the Western Escarpment of the Guadalupe Mountains using properties from outcrop, normal, and overpressured Gulf
Michael Batzle, Michael H. Gardner
openaire +1 more source
Abstract Lithology and fluid information can be extracted from seismic data of deepwater clastics if their relative contribution to the signal is understood. Brushy Canyon Formation outcrop seismic models are constructed for the Western Escarpment of the Guadalupe Mountains using properties from outcrop, normal, and overpressured Gulf
Michael Batzle, Michael H. Gardner
openaire +1 more source
Lithology Identification Using Lithology Impedance in Mumbai Offshore
2019The study area belongs to the marine geological setup of Surat depression of Mumbai Offshore Basin, India. The lithology of three wells in Mumbai offshore is analyzed using Gamma-Ray (GR) log, Density (ρ) log, Resistivity (Rt) log and Neutron Porosity (Φ) log. This analysis makes the identification of the lithology difficult.
Amrita Roy, Rima Chatterjee
openaire +1 more source

