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  • 1
    Publication Date: 2017-04-04
    Description: Travel times of about 39,000 Pn arrivals recorded from regional earthquakes by the Italian Telemetered Seismic Network and by stations of nearby countries are inverted to image lateral variations of seismic velocity and anisotropy at subcrustal depth in Italy and surrounding regions. This method allows simultaneous imaging of variations of Pn velocity and anisotropy, as well as crustal thickness variations. The Po plain, the Adriatic Sea, and the Ionian Sea have normal to high Pn velocities. In contrast, lower velocities (7.9-8.0 km/s) are imaged in Italy beneath the western Alps, the northern Apennines, and eastern Sicily and nearby Calabria, as well as in northern Albania and beneath the Pannonian basin. Low Pn velocities beneath the northern Apennines correlate with present-day extension and may have resulted from thermal anomalies in the uppermost mantle due to delamination processes. Low velocities are consistent with the high-attenuation zone inferred in the uppermost mantle beneath the internal Apennine units and the Tyrrhenian margin of the peninsula by Mele et al. [1996, 1997]. On the contrary, low velocities beneath the western Alps may be an apparent effect due to the abrupt thickening of the crustal roots. Pn velocity is anisotropic in the study area with a maximum amplitude of ± 0.2 km/s. The largest anisotropic velocity anomalies are observed along the major arc structures of Italy, i.e., the northern Apennines and the Calabrian Arc, indicating that these features are controlled by uppermost mantle processes. The anisotropy anomaly along the Calabrian Arc extends as far as Albania but ends abruptly north of this area, suggesting that a lithospheric discontinuity is present along the northern Albanian border.
    Description: Published
    Description: 12,529-12,543
    Description: JCR Journal
    Description: reserved
    Keywords: Pn anisotropic tomography ; Italy ; 04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Medical & biological engineering & computing 17 (1979), S. 563-568 
    ISSN: 1741-0444
    Keywords: First-heart-sound spectra ; Mitral-valve vibration ; Voiceprint spectrograph
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Medicine
    Notes: Abstract Heart-sound recording are taken from human and animal subjects. Spectral analysis of small time segments of the first heart sound is carried out by means of a spectrograph analyser. Temporal variations in the spectra are observed during the first major component of the first heart sound. Peak energy frequencies in the medium frequency range (50–140 Hz) are observed to increase in successive spectra during the first major component of the first-heart-sound, and also with the decrease in the size of the heart from which the recordings were made.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Medical & biological engineering & computing 20 (1982), S. 466-472 
    ISSN: 1741-0444
    Keywords: Echocardiogram ; Fast Fourier transform ; First heart sound ; Membrane vibration ; Mitral-leaflet closing velocity ; Phonocardiogram
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Medicine
    Notes: Abstract A mathematical model is presented to relate mitral valve leaflet closing velocity to the subsequent vibrational magnitude following valve closure. This relationship is investigated experimentally by means of phonocardiographic and echocardiographic recordings from 17 human subjects. Fast Fourier transform analysis of digitised first heart sounds from each subject reveals that the sound intensities in different frequency bands are not uniformly related to the valve-leaflet closing velocity, obtained from the anterior mitral leaflet echocardiogram. It is found that, in the frequency range up to 150 Hz, closing velocity correlates best with sound intensity in the 30–45 hz bandwidth.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 1989-03-01
    Print ISSN: 0022-1376
    Electronic ISSN: 1537-5269
    Topics: Geosciences
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  • 5
    Publication Date: 2014-11-07
    Description: The 127 station NorthEast China Extended SeiSmic Array (NECESSArray) provides large quantities of high quality seismic data in northeast China that allow us to resolve lateral variations of Lg Q or crustal attenuation at 1 Hz ( Q o ) to 2.0° or greater. Using the reverse two-station/event method with 11 642 Lg path-amplitudes from 78 crustal earthquakes, we obtain a 2-D tomographic image of Lg Q o with values ranging from ~50 to 1400. A high degree of detail in the lateral variation of Lg attenuation is revealed in our tomographic image. High Q o regions are found in the Great Xing'an, Lesser Xing'an and Songen-Zhangguangcai Ranges. Low Q o regions are observed in the Songliao, Sanjiang and Erlian Basins. The lowest Q o is found near the Wudalianchi volcanic field and other Quaternary volcanic fields, the southern Songliao Basin, the western edge of the Erlian Basin and the Sanjiang Basin. Low Q o values are measured for paths that cross sedimentary basins with thick, unconsolidated sediments. Most of the high Lg attenuation in the Songliao Basin correlates reasonably well with low crustal Rayleigh wave phase velocity anomalies. The highest attenuating regions also correlate well with regions of Holocene volcanism.
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 6
    Publication Date: 2019
    Description: 〈span〉〈div〉SUMMARY〈/div〉Using 〈span〉Pn〈/span〉-wave traveltimes from three regional distance ranges we generated 〈span〉Pn〈/span〉 tomography models to investigate the 3-D nature of the uppermost mantle lid 〈span〉P〈/span〉-wave velocity structure beneath the Tibetan Plateau and surrounding regions. Significant velocity variations spatially and with depth are observed. High-velocity regions are found beneath the Himalayas and most parts of southern Tibet. These high-velocity regions can be interpreted as subducting Indian continental mantle lithosphere, accreted terranes and a cold, non-convective mantle wedge beneath central Plateau. They are disjointed suggesting that the subducting Indian lithosphere is fragmented laterally. In the western Tibetan Plateau, the high-velocity region extends northwards to the middle of Qiangtang Terrane. In the central Plateau, the high-velocity region reaches near the Bangong–Nujiang suture. The northern extent of the subducted Indian continent cannot be determined uniquely from 〈span〉Pn〈/span〉 models because the Indian plate dips moderately beneath southeastern Tibet. Around the Plateau, Tarim, Qaidam, Gonghe and Sichuan basins are floored by high-velocity Asian continental blocks that keep the elevation of these basins lower than surrounding regions. We found no evidence of an ongoing southward subduction of Asian lithosphere beneath central to northeastern Tibetan Plateau. Two major 〈span〉Pn〈/span〉 low-velocity anomalies are found beneath northern and northeastern Tibet, primarily within the Qiangtang and Songpan-Ganzi Terranes. The northern Tibet low-velocity mantle is situated in a continental backarc of the India–Asia continental subduction zone, and hence we interpreted this region as thin thermal lithosphere with upwelling mantle driving by the subducting Indian lithosphere. The Qilianshan is also underlain by a low-velocity mantle structure and could be related to the same upwelling in this continental backarc. A narrow N–S trending low-velocity anomaly is found beneath the Yadong–Gulu Rift and confirmed that the Lhasa Terrane is not limited to the crust, but involves the entire lithosphere. Another pronounced low 〈span〉Pn〈/span〉 velocity region is observed in the southeastern Tibetan Plateau, southern Yunnan and northeastern Myanmar. This feature is probably related to backarc convection associated with the subduction and rollback of Indian oceanic slab beneath Myanmar and Yunnan province, China.International Seismological Centre, On-line Bulletin, 〈a href="http://www.isc.ac.uk/"〉http://www.isc.ac.uk〈/a〉, Internatl. Seismol. Cent., Thatcham, United Kingdom, 2016.〈/span〉
    Print ISSN: 2051-1965
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 7
    Publication Date: 2019
    Description: 〈span〉〈div〉Summary〈/div〉Using Pn-wave travel times from three regional distance ranges we generated Pn tomography models to investigate the three-dimensional nature of the uppermost mantle lid P-wave velocity structure beneath the Tibetan Plateau and surrounding regions. Significant velocity variations spatially and with depth are observed. High velocity regions are found beneath the Himalayas and most parts of southern Tibet. These high velocity regions can be interpreted as subducting Indian continental mantle lithosphere, accreted terranes, and a cold, non-convective mantle wedge beneath central Plateau. They are disjointed suggesting that the subducting Indian lithosphere is fragmented laterally. In the western Tibetan Plateau, the high velocity region extends northward to the middle of Qiangtang Terrane. In the central Plateau, the high velocity region it reaches near the Bangong-Nujiang Suture. The northern extend of the subducted Indian continent cannot be determined uniquely from Pn models because the Indian plate dips moderately beneath southeastern Tibet. Around the Plateau, Tarim, Qaidam, Gonghe, and Sichuan basins are floored by high velocity Asian continental blocks that keep the elevation of these basins lower than surrounding regions. We found no evidence of an ongoing southward subduction of Asian lithosphere beneath central to northeastern Tibetan Plateau. Two major Pn low velocity anomalies are found beneath northern and northeastern Tibet, primarily within the Qiangtang and Songpan-Ganzi Terranes. The northern Tibet low velocity mantle is situated in a continental back-arc of the India-Asia continental subduction zone, and hence we interpreted this region as thin thermal lithosphere with upwelling mantle driving by the subducting Indian lithosphere. The Qilianshan also underlain by a low velocity mantle structure and could be also related to the same upwelling in this continental back-arc. A narrow N-S trending low velocity anomaly is found beneath the Yadong-Gulu Rift (YGR) and confirmed that the Lhasa Terrane is not limited to the crust, but involves the entire lithosphere. Another pronounced low Pn velocity region is observed in the southeastern Tibetan Plateau, southern Yunnan and northeastern Myanmar. This feature is probably related to back-arc convection associated with the subduction and rollback of Indian oceanic slab beneath Myanmar and Yunnan province, China.〈/span〉
    Print ISSN: 2051-1965
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 8
    Publication Date: 1981-03-01
    Print ISSN: 0031-9155
    Electronic ISSN: 1361-6560
    Topics: Biology , Medicine , Physics
    Published by Institute of Physics
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