1,741,126 research outputs found
(Table 1) Summary of VPS correlations at ODP Site 126-792
No full textCorrelation of the logs from the Izu-Bonin forearc sedimentary sections at Sites 787, 792, and 793 with the core data from Holes 787A-787B, 792A-792E, and 793A-793B allows the development of a more detailed lithostratigraphic model for those sites, and a more precise correlation of lithologic boundaries to basin-wide seismic reflections. Early Oligocene arc volcanics form the basement strata (Unit 5) sampled at Sites 792 and 793. Downdropped and rotated blocks of Eocene forearc may form a sub-basement beneath these flows in the central forearc basin; mid-Eocene basement was recovered at Sites 782 and 786 on the outer-arc high during Leg 125. Basement at Site 792 was defined using the vertical seismic profile (VSP) and logging data. Deep reflectors observed on the vertical seismic profile may originate in the Eocene sub-basement. Thick sequences of coarse-grained volcaniclastic and hemipelagic sediment fill the 70- to 140-km-wide forearc sedimentary basin. Unrecovered (early Oligocene) strata beneath an unconformity, imaged by the multichannel seismic (MCS) line passing over Site 792, fill the deepest grabens of the central forearc and constitute Unit 4. The rapid deposition of volcaniclastics (Unit 3) during a dominant eruptive phase spanning much of the Oligocene, together with erosion of the basement highs bounding the basin, contributed to rapid subsidence and infilling. An inspection of cored materials from Unit 3 and logging data from Sites 792 and 793 reveals microfaults and other structural evidence for extension; on a much larger scale, MCS data show large normal faults near the frontal-arc high and outer-arc high that downfault the sediment section towards the central basin. Much of the largely pelagic or hemipelagic early Miocene section (Unit 2) has been removed by submarine valley formation and erosion, as at Sites 787 and 792. Middle Miocene to Holocene volcaniclastics and hemipelagics (Unit 1) top the forearc sedimentary section
SB 792
No full textSB 792, Introduced version -- SB 792-A, A-Engrossed version.Title from PDF caption (viewed on July 22, 2021).This archived document is maintained by the State Library of Oregon as part of the Oregon Documents Depository Program. It is for informational purposes and may not be suitable for legal purposes.Mode of access: Internet from the Oregon Government Publications Collection.Text in English
Santa Fe (ATSF) 792
No full textA photograph print showing Santa Fe (ATSF) 792, 2-8-0, (BLW) class 789, Cushing, OK
Santa Fe (ATSF) 792
No full textA photograph print showing Santa Fe (ATSF) 792, 2-8-0, (BLW) class 789, Cushing, OK
792. Kyōgen
No full textIwao Seiichi, Iyanaga Teizō, Ishii Susumu, Yoshida Shōichirō, Fujimura Jun'ichirō, Fujimura Michio, Yoshikawa Itsuji, Akiyama Terukazu, Iyanaga Shōkichi, Matsubara Hideichi. 792. Kyōgen. In: Dictionnaire historique du Japon, volume 13, 1987. Lettre K (3) pp. 151-152
Going Beyond Counting First Authors in Author Co-citation Analysis
Get PDFThe present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
- …
