1920x1080 pixel color camera with progressive scan at 50 to 60 frames per second

1998 ◽  
Author(s):  
William E. Glenn ◽  
John W. Marcinka
Keyword(s):  
Pixel Color ◽  
Progressive Scan

1920 × 1080 Pixel Color Camera with a Progressive Scan Output at 60 Frames/Sec

SMPTE Journal ◽  
1998 ◽  
Vol 107 (11) ◽  
pp. 947-949 ◽  
Author(s):  
William E. Glenn ◽  
John W. Marcinka
Keyword(s):  
Pixel Color ◽  
Progressive Scan

scholarly journals Constructing as-is BIMs from progressive scan data

2012 ◽  
Vol 11 (2) ◽  
Author(s):  
T. Gao ◽  
B. Akinci ◽  
S. Ergan ◽  
J. Garrett
Keyword(s):  
Scan Data ◽  
Progressive Scan

A progressive scan CCD image sensor for DSC applications

2000 ◽  
Vol 35 (12) ◽  
pp. 2044-2054 ◽  
Author(s):  
T. Yamada ◽  
K. Ikeda ◽  
Yong-Gwan Kim ◽  
H. Wakoh ◽  
T. Toma ◽  
...  
Keyword(s):  
Image Sensor ◽  
Ccd Image Sensor ◽  
Progressive Scan ◽  
Ccd Image

scholarly journals Coseismic Deformation Field of the Mw 7.3 12 November 2017 Sarpol-e Zahab (Iran) Earthquake: A Decoupling Horizon in the Northern Zagros Mountains Inferred from InSAR Observations

2018 ◽  
Vol 10 (10) ◽  
pp. 1589 ◽  
Author(s):  
Sanaz Vajedian ◽  
Mahdi Motagh ◽  
Zahra Mousavi ◽  
Khalil Motaghi ◽  
Eric. Fielding ◽  
...  
Keyword(s):  
Hanging Wall ◽  
Source Model ◽  
Lateral Spreading ◽  
Maximum Amount ◽  
Coseismic Deformation ◽  
Past Century ◽  
Zagros Mountains ◽  
Tectonically Active ◽  
Northern Portion ◽  
Progressive Scan

The study of crustal deformation fields caused by earthquakes is important for a better understanding of seismic hazard and growth of geological structures in tectonically active areas. In this study, we present, using interferometric measurements constructed from Sentinel-1 Terrain Observation with Progressive Scan (TOPS) data and ALOS-2 ScanSAR, coseismic deformation and source model of the Mw 7.3, 12 November 2017 earthquake that hit northwest of the Zagros Mountains in the region between Iran–Iraq border. This was one of the strongest seismic events to hit this region in the past century, and it resulted in an uplift area of about 3500 km2 between the High Zagros Fault (HZF) and Mountain Front Fault (MFF) with a maximum amount of 70 cm south of Miringe fault. A subsidence over an area of 1200 km2 with a maximum amount of 35 cm occurred near Vanisar village at the hanging wall of the HZF. Bayesian inversion of interferometric synthetic aperture radar (InSAR) observations suggests a source model at a depth between 14 and 20 km that is consistent with the existence of a decoupling horizon southwest edge of the northern portion of the Zagros Mountains near the MFF. Moreover, we present evidence for a number of coseismically induced rockslides and landslides, the majority of them which occurred along or close to pre-existing faults, causing decorrelation in differential interferograms. Exploiting the offset-tracking technique, we estimated surface motion by up to 34 and 10 m in horizontal and vertical directions, respectively, due to lateral spreading on a big coseismic-induced landslide near Mela-Kabod. Field observations also revealed several zones of en echelon fractures and crack zones developed along a pre-existing fault passing through Qasr-e Shirin City, which exhibited secondary surface slip by up to 14 cm along its strike.

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