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Geiger

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Journal Article
Published: 01 December 2002
Mineralogical Magazine (2002) 66 (6): 1107–1108.
... consists of fifteen chapters organized into five sections. Geiger provides a brief introduction in Part I followed by four chapters in Part II devoted to thermodynamic properties. Grimwall discusses the dependence of thermodynamic properties on bonding, laying the basis for later chapters linking atomic...
Journal Article
Published: 01 December 1963
Journal of Sedimentary Research (1963) 33 (4): 945–947.
...David S. Buist Abstract Utilizing NaF as an internal standard and MgO as a diluent, quantitative evaluation of the amount of rutile can be obtained by x-ray diffraction of beach sands with a Geiger detection method. The percentage obtained by the x-ray method was checked with chemical determination...
Journal Article
Journal: Economic Geology
Published: 01 May 1950
Economic Geology (1950) 45 (3): 245–248.
Journal Article
Journal: Geophysics
Published: 01 April 1944
Geophysics (1944) 9 (2): 180–216.
...William Low Russell Abstract Geiger counter determinations of the gamma ray intensity of 510 rock samples have been made to determine the average radioactivity and frequency distribution of radioactivities of the various types of sedimentary rocks. The results, expressed in units of gamma ray...
Journal Article
Published: 01 April 1937
Bulletin of the Seismological Society of America (1937) 27 (2): 109–112.
...John H. Hodgson Copyright © 1937, by the Seismological Society of America * Manuscript received for publication March 15, 1937. References 1 Geiger Ludwig Herdbestimmung bei Erdbeben aus den Ankunftszeiten...
Series: Society of Exploration Geophysicists Geophysics Reprint Series
Published: 01 January 2008
EISBN: 9781560801917
... into the correct spatial position for velocity analysis ( Ferber, 1994 ). After the gathers have been formed, NMO correction and stacking complete the prestack migration. Equivalent offset migration (EOM) ( Bancroft and Geiger, 1994 , 1997. 1998) forms prestack miration gathers similar to Gardner’s DMO-PSI...
Journal Article
Journal: Geophysics
Published: 26 May 2006
Geophysics (2006) 71 (3): S111–S120.
...Gary F. Margrave; Hugh D. Geiger; Saleh M. Al-Saleh; Michael P. Lamoureux Abstract We present a new approach to the design and implementation of explicit wavefield extrapolation for seismic depth migration in the space-frequency domain. Instability of the wavefield extrapolation operator...
FIGURES
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Histograms illustrating location error distributions produced by the Geiger method and the relative relocation method in (a) and (b) the horizontal direction and (c) and (d) the vertical direction.
Published: 01 January 2024
Figure 7. Histograms illustrating location error distributions produced by the Geiger method and the relative relocation method in (a) and (b) the horizontal direction and (c) and (d) the vertical direction.
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Microseismic location results using the Geiger approach. (a) Map view and cross-section views from the (b) y and (c) x axes of the acquisition. The red circles represent the true source locations. The blue crosses indicate the locations determined by the Geiger method.
Published: 01 January 2024
Figure 5. Microseismic location results using the Geiger approach. (a) Map view and cross-section views from the (b) y and (c) x axes of the acquisition. The red circles represent the true source locations. The blue crosses indicate the locations determined by the Geiger method.
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Comparison between the synthetic test hypocenter locations from the Geiger approach (original) and the application of the postprocessing collapsing technique (collapsed). The green crosses indicate the true source locations. The geometrical description of the fracture is enhanced by the postprocessing application of the collapsing method.
Published: 01 January 2024
Figure 8. Comparison between the synthetic test hypocenter locations from the Geiger approach (original) and the application of the postprocessing collapsing technique (collapsed). The green crosses indicate the true source locations. The geometrical description of the fracture is enhanced
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IR spectra of Mg3Al2Si3O12 (P-13; Geiger et al. 1991) synthesized at PH2O = 2.3 Ga and T = 1100 °C and garnet of composition (Mg2.50Fe0.592+)(Si0.06Al1.76Cr0.08Fe0.023+)Si3O12 (spectrum MA384 digitized from Thomas et al. 2015, with absorbance divided by 30) synthesized at PH2O = 18 GPa and T = 1800 °C (with 0.5 L H2O added). The OH– band defines a local hydropyrope cluster in both crystals.
Published: 01 March 2018
Figure 7. IR spectra of Mg 3 Al 2 Si 3 O 12 (P-13; Geiger et al. 1991 ) synthesized at P H 2 O = 2.3 Ga and T = 1100 °C and garnet of composition (Mg 2.50 Fe 0.59 2+ )(Si 0.06 Al 1.76 Cr 0.08 Fe 0.02 3+ )Si 3 O 12 (spectrum MA384 digitized from Thomas et al. 2015 , with absorbance
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Distribution of available measurements within the original Koeppen–Geiger classes (left) and the summarized classes (right).
Published: 01 May 2013
Fig. 3. Distribution of available measurements within the original Koeppen–Geiger classes (left) and the summarized classes (right).
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(A) Dynamic capillary pressure data from Geiger and Durnford (2000), and (B) fit of the experimental data to our model for dynamic capillary pressure; S is the suction head, q* and ηq/γ are nondimensional Darcy velocities, and 60–80, 80–100, and 100–140 are particle sizes according to the U.S. standard sieve size system.
Published: 01 May 2011
Fig. 3. (A) Dynamic capillary pressure data from Geiger and Durnford (2000) , and (B) fit of the experimental data to our model for dynamic capillary pressure; S is the suction head, q * and η q /γ are nondimensional Darcy velocities, and 60– 80, 80–100, and 100–140 are particle sizes
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DSC Cp data of Geiger & Voigtländer (2000, GV00) and PPMS Cp data between 250 and 300 K for anhydrous Fe- and Mg-cordierite. Fits to the data are shown as solid curves as described by Eqs. (2a) and (2b) in the text. The transition region between PPMS and DSC data is shown on an expanded scale in the inset, where the low-temperature adiabatic calorimetry (low-T AC) data of Paukov et al. (2006, P06) have also been plotted.
Published: 01 February 2008
Fig. 3. DSC C p data of Geiger & Voigtländer (2000 , GV00) and PPMS C p data between 250 and 300 K for anhydrous Fe- and Mg-cordierite. Fits to the data are shown as solid curves as described by Eqs. (2a) and (2b) in the text. The transition region between PPMS and DSC data is shown
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With a Geiger counter on hand, Barrow leads a field expedition to explore for uranium in Western Australia in 1974–75.
Published: 01 December 2003
Figure 3. With a Geiger counter on hand, Barrow leads a field expedition to explore for uranium in Western Australia in 1974–75.
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Figure 4. Explanation of the Geiger-Delaunay reconstruction technique. A, A contour C1 in the plane P1. B, Final Delaunay triangulation of the original and added points in the contour C1. C, A contour C2 in the plane P2. D, Final Delaunay triangulation of the original and added points in the contour C2. E, Tetrahedron of type t1. F, Tetrahedron of type t2. G, Tetrahedron of type t12. H, Reconstruction based upon contour C1 in plane P1 (lower) and contour C2 in plane P2 (top), where all unobstructed connecting lines (i.e., sides of tetrahedrons) on the exterior are shown. I, The same reconstruction except where all connecting lines on the exterior are shown. J, Fully rendered reconstruction composed of opaque triangles, based upon contour C1 in plane P1 (lower) and contour C2 in plane P2 (top)
Published: 01 January 2001
Figure 4. Explanation of the Geiger-Delaunay reconstruction technique. A, A contour C 1 in the plane P 1 . B, Final Delaunay triangulation of the original and added points in the contour C 1 . C, A contour C 2 in the plane P 2 . D, Final Delaunay triangulation of the original and added
Journal Article
Published: 01 April 1984
Bulletin of the Seismological Society of America (1984) 74 (2): 655–667.
...D. Caccamo; G. Neri Abstract A new procedure for locating local earthquakes is proposed. Essentially, this procedure consists in solving—by means of least-squares technique—a system of equations which is formally analogous to that of Geiger ( Ax = b ) but different from his in the values...
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The (a) isobaric and (b) isothermal mode Grüneisen parameters as well as the intrinsic anharmonic parameters (c) for the olivine samples of Fo100 (Chopelas 1990; Gillet et al. 1991; Kolesov and Geiger 2004; Hushur et al. 2009), Fo89Fa11 (Kolesov and Geiger 2004; this study) and Fo58Fa42 (this study).
Published: 01 October 2021
Figure 8. The ( a ) isobaric and ( b ) isothermal mode Grüneisen parameters as well as the intrinsic anharmonic parameters ( c ) for the olivine samples of Fo 100 ( Chopelas 1990 ; Gillet et al. 1991 ; Kolesov and Geiger 2004 ; Hushur et al. 2009 ), Fo 89 Fa 11 ( Kolesov and Geiger 2004
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Atomic amplitudes of vibration for a given EO8 coordination for different end-member garnets as calculated from the difference between their atomic mean-square displacements at 500/550 and 100 K. The projections are approximately along twofold axes and those in the right-hand column are rotated approximately 90° from the projections in the left-hand column. The E-cation shows anisotropic thermal vibration (i.e., dynamic disorder) with the largest amplitude in the plane of the longer E-O4 bonds. The eight surrounding oxygen anions have smaller vibrational amplitudes (from Geiger et al. 1992; Armbruster et al. 1992; Armbruster and Geiger 1993; Geiger and Armbruster 1997).
Published: 01 April 2013
are rotated approximately 90° from the projections in the left-hand column. The E -cation shows anisotropic thermal vibration (i.e., dynamic disorder) with the largest amplitude in the plane of the longer E -O4 bonds. The eight surrounding oxygen anions have smaller vibrational amplitudes (from Geiger et
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Figure 3. Size distributions of living abalone taxa by regions. Box plots display sample medians and quartiles; * = outliers. Size data from Lindberg (1992), Geiger (1998, 2000), and Hutsell et al. (1999); distributional data from Geiger (2000)
Published: 01 January 2005
Figure 3. Size distributions of living abalone taxa by regions. Box plots display sample medians and quartiles; * = outliers. Size data from Lindberg (1992) , Geiger (1998 , 2000 ), and Hutsell et al. (1999) ; distributional data from Geiger (2000)