PDF-Velocity model building for tilted orthorhombic depth imaging Yunfeng

121212121212121212121222113223222022 Figure 1 Comparison of tilted transverse isotropy TTI with tiltedorthorhombic TORT a TTI stress and wave are symmetrical inx. in Data Streams . at Multiple Time Granularities. CS525 Paper Presentation. Presented by:. Pei Zhang, . Jiahua. Liu, . Pengfei. . Geng. and . Salah. Ahmed. Authors: Chris . Giannella. , . Jiawei. Continental cratons - cold, rigid material. Spreading centers & mountains - warm mantle. P. ,. S, and Q. Tomography - Tonga Arc. Velocity tomography shows anomalies relative to average model [. Conder and Wiens. Yasuhiro Mukaigawa (Osaka University). Seiichi Tagawa (Osaka University). Jaewon Kim (MIT Media Lab). Ramesh Raskar (MIT Media Lab). Yasuyuki Matsushita (Microsoft Research Asia). Yasushi Yagi (Osaka University). Figure 2The workflow for orthorhombic model building. DOI http://dx.doi.org/10.1190/segam2013-0968.1 Receiver Functions. Body Wave Tomography. Surface (Rayleigh) wave tomography. Good for: Imaging discontinuities. . (. Moho. , . sed. /rock interface, 410). Weakness: can’t see gradients. . can’t constrain velocities well. of . Electromagnetic and Seismic . Wavefields. . International Symposium on Geophysical Imaging . with . Localized Waves. Sanya. , . Hainin. Island China. July 24-28, 2011. Gregory A. Newman. Earth Sciences Division. Jason Howard, Natalie . Holzwarth. Acknowledgements . Zach Hood. WFU . Deac. HPC Cluster . NSF grant DMR-1507942 . Outline. Motivation. Background of material. Low temperature phase structure search. Computational . Imaging. Oliver . Cossairt. PhD. Thesis Proposal. 5/3/2011. How do we measure the visual world?. What is measurable?. The . Plenoptic. Function. What do we measure?. p. e. -. e. -. e. Continental cratons - cold, rigid material. Spreading centers & mountains - warm mantle. P. ,. S, and Q. Tomography - Tonga Arc. Velocity tomography shows anomalies relative to average model [. Conder. You can see it on a. . . position time . graph OR. a . velocity time . graph. POSITION v TIME. Velocity is seen by the . slope. Graphing motion. position-time. Section 1 on graph represents biker going forward. Changes in . Spoken Language. What can you tell about the man from this extract?. From Dickens’s . Great Expectations . (1860), . ch. . 1:. After darkly looking at his leg and me several times, he came closer to my tombstone, took me by both arms, and tilted me back as far as he could hold me; so that his eyes looked most powerfully down into mine, and mine looked most helplessly up into his. . Modified by: Jeff Kitchen, CA WSC. Control. Measurement Section. W. 5W. 2W. Site Selection . The channel should be straight and uniform for a distance long enough to support uniform flow.. Riffle. Flow. Adrenal glands can be affected by a variety of lesions. Adrenal lesions can either be primary, of adrenal origin, or secondary to other pathologies. Primary adrenal lesions can further be either of cortical or medullary origin. Functioning adrenal lesions can also give clues to the histologic diagnosis and direct workup. Over the years, various imaging techniques have been developed that have increased diagnostic accuracy and helped in better characterization of adrenal lesions non-invasively. In the first part of the two part series, we review adrenal imaging techniques and adrenal cortical tumors such as adenomas, adrenocortical tumors, adrenal hyperplasia and oncocytomas. In physics, . velocity . is speed in a . given direction. . . When we say a car travels at 60 km/h, we are specifying its speed. . When we say a car moves at 60 km/h to the . north. , we are specifying its velocity..