NMR well logging at Schlumberger
暂无分享,去创建一个
[1] Mark A. Horsfield,et al. Transverse relaxation processes in porous sedimentary rock , 1990 .
[2] J. Howard,et al. Nmr In Partially Saturated Rocks: Laboratory Insights On Free Fluid Index And Comparison With Borehole Logs , 1995 .
[3] J. Banavar,et al. Surface relaxation and pore sizes in rocks ― a nuclear magnetic resonance analysis , 1986 .
[4] C. Straley,et al. SPE 26470 Nuclear Magnetic ResonaFlce of Rocks: T1 vs. T2 , 1993 .
[5] Joseph Klafter,et al. Molecular dynamics in restricted geometries , 1989 .
[6] D I Hoult,et al. The signal-to-noise ratio of the nuclear magnetic resonance experiment. 1976. , 1976, Journal of magnetic resonance.
[7] K. Brownstein,et al. Importance of classical diffusion in NMR studies of water in biological cells , 1979 .
[8] K. H. Lee,et al. Interpretation of water nuclear magnetic resonance relaxation times in heterogeneous systems , 1974 .
[9] David P Gallegos,et al. A NMR technique for the analysis of pore structure: Determination of continuous pore size distributions , 1988 .
[10] R. Freedman,et al. An Improved Nmr Tool Design For Faster Logging , 1999 .
[11] J. A. Jackson,et al. Remote (inside-out) NMR. III. Detection of nuclear magnetic resonance in a remotely produced region of homogeneous magnetic field , 1980 .
[12] Z. Taicher,et al. A comprehensive approach to studies of porous media (rocks) using a laboratory spectrometer and logging tool with similar operating characteristics. , 1994, Magnetic resonance imaging.
[13] Very Rapid Simultaneous Measurement of Nuclear Magnetic Resonance Spin-Lattice Relaxation Time and Spin-Spin Relaxation Time , 1991 .
[14] D. D. Griffin,et al. Novel NMR apparatus for investigating an external sample , 1992 .
[15] J. A. Jackson,et al. Remote (inside-out) NMR. II. Sensitivity of NMR detection for external samples , 1980 .
[16] D. Woessner,et al. N.M.R. SPIN-ECHO SELF-DIFFUSION MEASUREMENTS ON FLUIDS UNDERGOING RESTRICTED DIFFUSION , 1963 .
[17] Robert L. Kleinberg,et al. Nuclear Magnetic Resonance of Rocks: T1 vs. T2 , 1993 .
[18] J. Robinson,et al. Relations Between Pore Size Fluid and Matrix Properties, and NML Measurements , 1970 .
[19] E. Purcell,et al. Relaxation Effects in Nuclear Magnetic Resonance Absorption , 1948 .
[20] Chris Morriss,et al. Core Analysis By Low-field Nmr , 1997 .
[21] Terizhandur S. Ramakrishnan,et al. Forward Models For Nuclear Magnetic Resonance In Carbonate Rocks , 1998 .
[22] Weng Cho Chew,et al. Noncontacting electrical conductivity sensor for remote, hostile environments , 1989 .
[23] N. Bloembergen,et al. Overhauser Effect in Manganese Solutions in Low Magnetic Fields , 1958 .
[24] RF Sensor of a Novel NMR Apparatus , 1993 .
[25] Kleinberg,et al. Effect of Paramagnetic Ions on NMR Relaxation of Fluids at Solid Surfaces , 1996, Journal of magnetic resonance. Series A.
[26] R. Ehrlich,et al. Pore-Size Distribution And NMR In Microporous Cherty Sandstones , 1989 .
[27] Abdurrahman Sezginer,et al. Nuclear magnetic resonance properties of rocks at elevated temperatures , 1992 .
[28] Partha P. Mitra,et al. Mechanism of NMR Relaxation of Fluids in Rock , 1994 .
[29] W. E. Kenyon,et al. A Three-Part Study of NMR Longitudinal Relaxation Properties of Water-Saturated Sandstones , 1988 .
[30] Richard K. Cooper,et al. Remote (inside-out) NMR. I. Remote production of region of homogeneous magnetic field☆ , 1980 .