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Book Chapter

VENADO SANDSTONE AT MONTICELLO DAM 52 Available to Purchase

Author(s)
Donald R. Lowe
Book: DEEP-WATER SANDSTONES: SUBMARINE CANYON TO BASIN PLAIN, WESTERN CALIFORNIA
Series: Guidebook
Publisher: Pacific Section American Association of Petroleum Geologists
Published: 01 January 2004
DOI: 10.32375/2004-GB79.9
EISBN: 9781733984416
... the west side of the Sacramento Valley and location of Fig. 12-1B . Colors same as in Fig. 3-1 . (B) Map of Monticello Dam and Cache Creek areas, western Sacramento Valley. Along the southern two thirds of the Sacramento Valley, the GVG includes Upper Cretaceous rocks totaling over 6000 m (19,600...
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Journal Article

Mechanism of Initial Seismicity Following Impoundment of the Monticello Reservoir, South Carolina Available to Purchase

Linyue Chen, Pradeep Talwani
Published: 01 December 2001
Bulletin of the Seismological Society of America (2001) 91 (6): 1582–1594.
DOI: https://doi.org/10.1785/0120000293
...Linyue Chen; Pradeep Talwani Abstract Induced seismicity has been observed near Monticello Reservoir, South Carolina, since December 1977. Deployment of a seismic network before impoundment allowed for detection and accurate location of pursuant seismicity since its inception. Corroborative fault...
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Journal Article

Renewed Seismicity near Monticello Reservoir, South Carolina, 1996–1999 Available to Purchase

Linyue Chen, Pradeep Talwani
Published: 01 February 2001
Bulletin of the Seismological Society of America (2001) 91 (1): 94–101.
DOI: https://doi.org/10.1785/0120000083
...Linyue Chen; Pradeep Talwani Abstract A surprising increase in seismicity started in and around Monticello Reservoir, South Carolina in December 1996, and by the end of 1999, over 700 earthquakes with –0.4 ≤ M L ≤ 2.5 had been located. This seismicity occurred in a new hypocentral region and filled...
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Journal Article

The role of elastic, undrained, and drained responses in triggering earthquakes at Monticello Reservoir, South Carolina Available to Purchase

Kusala Rajendran, Pradeep Talwani
Published: 01 August 1992
Bulletin of the Seismological Society of America (1992) 82 (4): 1867–1888.
DOI: https://doi.org/10.1785/BSSA0820041867
... to the availability of detailed seismicity and geological and in situ stress data at Monticello Reservoir, it was possible to study various factors that control the mechanism of reservoir-induced seismicity. Our results suggest that, during the filling period, the instability resulted from elastic, undrained...
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Journal Article

Depth dependence of source parameters at Monticello, South Carolina Available to Purchase

J. B. Fletcher, J. Boatwright, W. B. Joyner
Published: 01 December 1983
Bulletin of the Seismological Society of America (1983) 73 (6A): 1735–1751.
DOI: https://doi.org/10.1785/BSSA07306A1735
...J. B. Fletcher; J. Boatwright; W. B. Joyner Abstract Three estimates of stress differences, which include Brune stress drop, stress drop from rms of acceleration ( a rms ), and the apparent stress, have been determined for 13 earthquakes at Monticello, South Carolina, a site of reservoir-induced...
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Journal Article

Late Quaternary eolian and alluvial response to paleoclimate, Canyonlands, southeastern Utah Available to Purchase

Marith C. Reheis, Richard L. Reynolds, Harland Goldstein, Helen M. Roberts, James C. Yount, Yarrow Axford, Linda Scott Cummings, Nancy Shearin
Journal: GSA Bulletin
Published: 01 July 2005
GSA Bulletin (2005) 117 (7-8): 1051–1069.
DOI: https://doi.org/10.1130/B25631.1
...) . Wells et al. (1990) suggested that this period of dune formation extended from before this date to some time after, noting a reported age of ca. 19 cal ka on bone at the base of a loess unit near Monticello ( Price et al., 1988 ). However, loess deposition need not coincide with sand deposition...
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Journal Article

Discovery of dermal spines reveals a new look for sauropod dinosaurs Available to Purchase

Stephen A. Czerkas
Journal: Geology
Published: 01 December 1992
Geology (1992) 20 (12): 1068–1070.
DOI: https://doi.org/10.1130/0091-7613(1992)020<1068:DODSRA>2.3.CO;2
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Journal Article

Geology of Cuba Available to Purchase

J. Whitney Lewis
Journal: AAPG Bulletin
Published: 01 June 1932
AAPG Bulletin (1932) 16 (6): 533–555.
DOI: https://doi.org/10.1306/3D932A90-16B1-11D7-8645000102C1865D
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Journal Article

Attenuation and backscattering from local coda Available to Purchase

Anton M. Dainty, Robert M. Duckworth, An Tie
Published: 01 October 1987
Bulletin of the Seismological Society of America (1987) 77 (5): 1728–1747.
DOI: https://doi.org/10.1785/BSSA0770051728
...Anton M. Dainty; Robert M. Duckworth; An Tie Abstract Coda decay and excitation for local events were examined at Mammoth Lakes and Morgan Hill, California, Monticello, South Carolina, and New Brunswick, Canada, in the frequency range of 3 to 50 Hz. The single-scattering theory of attenuation...
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Image
“Section of the mountains of Coregna, Monticello and Campiglia”. Watercolor drawn by Capellini attached to the manuscript “Some observations about the fossil localities and the stratigraphy of the Jurassic terrain in the western chain of mountains of La Spezia to Pisa”. Academia Lunigianese, Capellini Archive in La Spezia, Collection Perlini. Coregna, Monticello and Campiglia are three hills on the southwest side of the city of La Spezia.

“Section of the mountains of Coregna, Monticello and Campiglia”. Watercolor... Available to Purchase

Published: 01 April 2014
Figure 4. “Section of the mountains of Coregna, Monticello and Campiglia”. Watercolor drawn by Capellini attached to the manuscript “Some observations about the fossil localities and the stratigraphy of the Jurassic terrain in the western chain of mountains of La Spezia to Pisa”. Academia
Image
The study area near Lake Monticello, shown as the small rectangle in Figure 1. The thin line shows the approximate shoreline of the reservoir. The filled triangles indicate reservoir-induced earthquake epicenters. Three-component station jsc is shown by the filled circle.

The study area near Lake Monticello, shown as the small rectangle in Figur... Available to Purchase

Published: 01 June 2003
Figure 3. The study area near Lake Monticello, shown as the small rectangle in Figure 1 . The thin line shows the approximate shoreline of the reservoir. The filled triangles indicate reservoir-induced earthquake epicenters. Three-component station jsc is shown by the filled circle.
Image
Example of a synthetic three-component Monticello Dam SV scattering function with normalized velocity waveforms on the left and Fourier velocity spectra on the right for the components as labeled.

Example of a synthetic three-component Monticello Dam S V scattering fun... Available to Purchase

Published: 01 December 2001
Figure 15. Example of a synthetic three-component Monticello Dam S V scattering function with normalized velocity waveforms on the left and Fourier velocity spectra on the right for the components as labeled.
Image
Another example of a synthetic three-component Monticello Dam SV scattering function with normalized velocity waveforms on the left and Fourier velocity spectra on the right for the components as labeled.

Another example of a synthetic three-component Monticello Dam S V scatte... Available to Purchase

Published: 01 December 2001
Figure 16. Another example of a synthetic three-component Monticello Dam S V scattering function with normalized velocity waveforms on the left and Fourier velocity spectra on the right for the components as labeled.
Image
Monticello Dam left abutment three-component broadband velocity waveforms from two 3 March 1998 M ∼1.8 blind thrust earthquakes located 5 km northwest of the Monticello Dam at an elevation of -11 km. The P- and S-wave direct arrivals from each earthquake are labeled as EQ1 and EQ2. The vertical line and small arrow show the travel-time delay of the slow S wave on the east component (bottom) relative to the fast S wave on the north horizontal component (middle).

Monticello Dam left abutment three-component broadband velocity waveforms f... Available to Purchase

Published: 01 December 2001
Figure 17. Monticello Dam left abutment three-component broadband velocity waveforms from two 3 March 1998 M ∼1.8 blind thrust earthquakes located 5 km northwest of the Monticello Dam at an elevation of -11 km. The P- and S- wave direct arrivals from each earthquake are labeled as EQ1
Image
S-wave time windows from the Monticello Dam north abutment, three-component broadband velocity waveforms are shown on the left from the 11 November 1997, 13:00 UTC, ML 3.5 earthquake located at 39.674° N, 122.146° W at an elevation of –17 km. Corresponding acceleration spectra are plotted on the right. The earthquake was located ∼130-km north of the dam between Willows and Orland. The S “Fmax” labels and arrows on the horizontal components show that S-wave attenuation is relatively low for frequencies up to about 6 Hz. Units are in counts since only the spectral shapes are of interest.

S -wave time windows from the Monticello Dam north abutment, three-componen... Available to Purchase

Published: 01 December 2001
Figure 25. S -wave time windows from the Monticello Dam north abutment, three-component broadband velocity waveforms are shown on the left from the 11 November 1997, 13:00 UTC, M L 3.5 earthquake located at 39.674° N, 122.146° W at an elevation of –17 km. Corresponding acceleration spectra
Image
Shows locations of initial seismicity to January 1978 at Monticello Reservoir. Insets show the location of the reservoir in south Carolina and the seismic stations used to locate the earthquakes. Open and solid circles show locations of earthquakes where the undrained effect due to impoundment of the reservoir resulted in weakening and strengthening, respectively. Boxed groups of epicenters and related fault-plane solutions for various locations are from Talwani and Acree (1987). X shows the location of the earthquake showing the largest strengthening. The stippled area shows the deepest part of the reservoir where no initial seismicity was observed. W1 shows the location of deep borehole 1.

Shows locations of initial seismicity to January 1978 at Monticello Reservo... Available to Purchase

Published: 01 December 2001
Figure 1. Shows locations of initial seismicity to January 1978 at Monticello Reservoir. Insets show the location of the reservoir in south Carolina and the seismic stations used to locate the earthquakes. Open and solid circles show locations of earthquakes where the undrained effect due
Image
Comparison of filling curve of Monticello Reservoir and initial seismicity to January 1978. Seismicity began about three weeks after the beginning of impoundment.

Comparison of filling curve of Monticello Reservoir and initial seismicity ... Available to Purchase

Published: 01 December 2001
Figure 2. Comparison of filling curve of Monticello Reservoir and initial seismicity to January 1978. Seismicity began about three weeks after the beginning of impoundment.
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Annual number of earthquakes recorded at Monticello Reservoir from 1977 to 1999. The horizontal line shows the seismicity level before impoundment.

Annual number of earthquakes recorded at Monticello Reservoir from 1977 to ... Available to Purchase

Published: 01 February 2001
Figure 1. Annual number of earthquakes recorded at Monticello Reservoir from 1977 to 1999. The horizontal line shows the seismicity level before impoundment.
Image
Shows locations of earthquakes (asterisks) at Monticello Reservoir from 15 December 1996 to 31 December 1999. Four of the 27 events that occurred ∼10 km SE to the reservoir are shown, and the other 23 are outside the area covered by the figure. Inset shows the location of the reservoir area in South Carolina. Also shown are the locations of two deep wells (W1 and W2) and Virgil C. Summer Nuclear Station (solid square). The seismic stations used to located the events are shown by triangles. MR02 is located about 9 km SSE of station jsc and is shown by a small square in the inset.

Shows locations of earthquakes (asterisks) at Monticello Reservoir from 15 ... Available to Purchase

Published: 01 February 2001
Figure 2. Shows locations of earthquakes (asterisks) at Monticello Reservoir from 15 December 1996 to 31 December 1999. Four of the 27 events that occurred ∼10 km SE to the reservoir are shown, and the other 23 are outside the area covered by the figure. Inset shows the location of the reservoir
Image
Semimonthly number of earthquakes in the Monticello Reservoir area from 1996 to 1999. Episodes of intense activity are shown by the horizontal bars.

Semimonthly number of earthquakes in the Monticello Reservoir area from 199... Available to Purchase

Published: 01 February 2001
Figure 3. Semimonthly number of earthquakes in the Monticello Reservoir area from 1996 to 1999. Episodes of intense activity are shown by the horizontal bars.