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Cape Sines

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Map of the <b>Cape</b> <b>Sines</b> continental slope transect. All stations, sampled in ...
Published: 01 January 2012
Figure 1. Map of the Cape Sines continental slope transect. All stations, sampled in September 2006, are marked in black circles.
Journal Article
Published: 08 August 2017
Canadian Journal of Earth Sciences (2017) 54 (9): 936-960.
... of the basinal shale and carbonate platform facies. Building on earlier graptolite work, 180 samples were collected from nine sections of the Cape Phillips Formation, of which 118 yielded approximately 7600 conodont elements representing 54 species in 25 genera, including one new genus and species, Mayrodus...
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Journal Article
Journal: Geology
Published: 01 June 2004
Geology (2004) 32 (6): 517-520.
... as the sole control on flexural profiles, which are modeled as dampened sine curves with wavelengths and magnitudes controlled by a number of physical parameters of the lithosphere and the applied loads. Basement tectonics is shown here to be an equally important control on the scale and shape of flexural...
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Journal Article
Published: 01 December 2009
Bulletin of Canadian Petroleum Geology (2009) 57 (4): 449-471.
... time series constructed from summed sine waves representing orbital periods for the eccentricity, obliquity and precession-index as predicted for late Viséan time. The introduction of significant new macrofaunal elements in the Windsor Group accompanied transgressions separated in time by 2.2 to 2.4...
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Journal Article
Published: 01 September 2013
Journal of the Geological Society (2013) 170 (5): 707-710.
... . 85 myr), with a mean frequency of 2.6 myr. Long-period orbital time series predicted through the Phanerozoic are used to generate sine waves to test against these data; the null hypothesis of no orbital influence is rejected with a high confidence level. Cooling episodes appear most frequent through...
FIGURES
Series: SEPM Special Publication
Published: 01 January 2012
DOI: 10.2110/pec.12.102.0195
EISBN: 9781565763135
... at nearby promontory Cape Verde indicates that there is an erosional surface at the base of the cliff face that corresponds to the erosional contact below Steno. The erosional contact at the base of Cape Verde lies at a lower elevation, but within the same plane as the contact below Steno, which indicates...
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Journal Article
Published: 01 December 2008
South African Journal of Geology (2008) 111 (4): 409-420.
... methods. Apatite grains were mounted in epoxy resin, polished and etched with 7% HNO 3 at 21°C for 50 s. Irradiation was carried out at the ANSTO facility, Lucas Heights, Australia. Microscopic analysis was completed at the University of Cape Town using an optical microscope with a computer driven stage...
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Journal Article
Published: 05 January 2016
Bulletin of the Seismological Society of America (2016) 106 (1): 1-12.
...Núria Romeu Petit; Yolanda Colom Puyané; José Antonio Jara Salvador; Xavier Goula Suriñach; Teresa Susagna Vidal Abstract The main aim of this study is to demonstrate the feasibility of an earthquake early warning system ( EEWS ) to warn of potentially destructive earthquakes in the Cape San...
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Journal Article
Published: 29 April 2016
Canadian Journal of Earth Sciences (2016) 53 (9): 931-949.
...Shunxin Zhang; Khusro Mirza; Christopher R. Barnes Abstract The conodont biostratigraphy for the Upper Ordovician – Upper Silurian carbonate shelf (Irene Bay and Allen Bay formations) and interfingering basinal (Cape Phillips Formation) facies is established for parts of Devon and Ellesmere islands...
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Image
Potential temperature-salinity diagram constructed from CTD measurements al...
Published: 01 January 2012
Figure 2. Potential temperature-salinity diagram constructed from CTD measurements along the Cape Sines transect. Temperature and salinity measurements for the Mediterranean Water (MW) at Gibraltar, and North East Atlantic Deep Water (NEADW) and Lower Deep Water (LDW) at the western Iberian
Image
Figures 1–3.  Uvigerina celtica  n. sp. Surface sample PO201/10-701 off Gal...
Published: 01 October 2006
peregrina (figure 14).
 Figures 12, 13. Uvigerina peregrina parva Lutze 1986 . Surface sample PO200/10-4-1 off Cape Sines, southern Portugal (37.330 ° N, 9.510 ° W, 1265 m water depth), size fraction > 250 μm. Note the distinctively higher and more serrate costae compared to specimens 4 and 5
Journal Article
Published: 01 January 2012
Journal of Foraminiferal Research (2012) 42 (1): 66-81.
...Figure 1. Map of the Cape Sines continental slope transect. All stations, sampled in September 2006, are marked in black circles. ...
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Journal Article
Published: 01 October 2000
Bulletin of the Seismological Society of America (2000) 90 (5): 1342-1348.
...Jian Zhang; Nicos Makris 29 9 1999 Copyright © 2000 by the Seismological Society of America 2000 The above-titled article presented response-time histories and spectra for the minimum acceleration amplitude of a full sine pulse that is needed to overturn a rigid, rectangular...
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Journal Article
Published: 01 May 2012
American Mineralogist (2012) 97 (5-6): 951-961.
... is based on the energy of the Fe L α peak ( Fialin et al. 2001 , 2004 ). Peak energies can, of course, be related to the geometry of the EMP spectrometer via Bragg’s law. In practice we describe peak energies in terms of the θ angle in Bragg’s law and herein are reported in units of sine θ. Thus, we...
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Journal Article
Published: 23 August 2017
Seismological Research Letters (2017) 88 (6): 1499-1507.
... 42 3 Lorca 44 6 Seville 45 6 23 January 2016 M w  4.5 southwest of Cape St. Vincent Faro −11 −45 Sines −9 −44 Lisbon 7 −29 Huelva 7 −26 Évora 11 −22 Cádiz 19 −17 Seville 26 −8 Badajoz 28 −5 Ceuta 41 2 Cáceres 45 13...
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Journal Article
Journal: Geophysics
Published: 24 August 2012
Geophysics (2012) 77 (5): R217-R225.
.... (a) Model for the sine curve exploding reflector with amplitude of 25 m and wavelength of 500 m in a constant velocity media of 2000     m / s . (b) Seismogram corresponding to the model in (a). The white dashed line maps a real diffraction at the corresponding peak. Peaks and troughs...
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Journal Article
Published: 01 October 2007
Bulletin of the Seismological Society of America (2007) 97 (5): 1486-1501.
... combination of sine waves, each representing a signal of infinite length and a single frequency. In contrast, wavelet analysis decomposes a signal into wavelets that are localized in time and that represent a narrow range of frequencies. For nonstationary signals such as earthquake ground motions, it can...
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Journal Article
Published: 01 March 2016
South African Journal of Geology (2016) 119 (1): 91-98.
... resolution of the system, whereas broadband noise (up to 10 kHz from the centre frequency) affects the overall system signal to noise ratio (SNR). Phase noise can also be described as the short-term random fluctuations of the frequency of the sine/square wave. The properties of this oscillator compare...
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Journal Article
Published: 01 October 2006
Journal of Foraminiferal Research (2006) 36 (4): 355-367.
... peregrina (figure 14).
 Figures 12, 13. Uvigerina peregrina parva Lutze 1986 . Surface sample PO200/10-4-1 off Cape Sines, southern Portugal (37.330 ° N, 9.510 ° W, 1265 m water depth), size fraction > 250 μm. Note the distinctively higher and more serrate costae compared to specimens 4 and 5...
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Journal Article
Published: 10 May 2016
Bulletin of the Seismological Society of America (2016) 106 (3): 1011-1023.
... Period Pulse Type * 1 540 N. Palm Springs 1986 WWT180 0.39 0.67 P s1 2 765 Loma Prieta 1989 G01090 0.54 1.16 P s1 3 776 Loma Prieta 1989 HSP000 0.42 2.18 P n1 4 779 Loma Prieta 1989 LGP000 0.48 2.55 P n1 5 825 Cape Mendocino 1992 CPM000 0.73...
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