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Tama River

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Location of the <span class="search-highlight">Tama</span> <span class="search-highlight">river</span> and investigation points (Station 1 and 2).
Published: 01 September 2002
FIGURE 1 Location of the Tama river and investigation points (Station 1 and 2).
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. Schematic cross_section of the sampling location at the <span class="search-highlight">Tama</span> <span class="search-highlight">river</span>.
Published: 01 September 2002
FIGURE 2 . Schematic cross_section of the sampling location at the Tama river.
Journal Article
Published: 01 September 2002
Environmental Geosciences (2002) 9 (3): 109–114.
...FIGURE 1 Location of the Tama river and investigation points (Station 1 and 2). ...
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Vertical grain size distribution of the core TMB collected from the <span class="search-highlight">Tama</span> ri...
Published: 01 September 2002
FIGURE 3 Vertical grain size distribution of the core TMB collected from the Tama river estuary on July 30, 1999. Three types of sediments were separated by a wet method (Zhao and Zhang, 1990): 2.00–0.063 mm (sand), 0.063–0.005 mm (silt), and <0.005 mm (mud).
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Model of In(OH) 3(s)  solubility at 25°C as a function of pH in the Kusatsu...
Published: 01 November 2013
−2.0 –10 −2.1 mol/L, F − concentrations: 10 −3.3 –10 −3.7 mol/L, SO 4 2− concentrations: 10 −1.9 –10 −2.2 mol/L. (B) Tamagawa study area: Modeling assumed Cl − , F − , and SO 4 2− concentrations of 10 −2.8 , 10 −4.3 , and 10 −3.0 mol/L, respectively; Cl − concentrations in the Tama River: 10
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Vertical geologic section along the <span class="search-highlight">Tama</span> Kosi <span class="search-highlight">River</span>. Approximate distributi...
Published: 01 April 2012
Figure 4. Vertical geologic section along the Tama Kosi River. Approximate distribution of metamorphic index minerals is shown. See Figure 3 for lithologic legend. Dashed lines indicate interpreted eroded unit contacts. Dotted lines indicate interpreted structural fabric orientation.
Journal Article
Journal: Economic Geology
Published: 01 November 2013
Economic Geology (2013) 108 (7): 1641–1656.
... −2.0 –10 −2.1 mol/L, F − concentrations: 10 −3.3 –10 −3.7 mol/L, SO 4 2− concentrations: 10 −1.9 –10 −2.2 mol/L. (B) Tamagawa study area: Modeling assumed Cl − , F − , and SO 4 2− concentrations of 10 −2.8 , 10 −4.3 , and 10 −3.0 mol/L, respectively; Cl − concentrations in the Tama River: 10...
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Geologic map of the <span class="search-highlight">Tama</span> Kosi-Rolwaling Himalaya. The section depicted in  ...
Published: 01 April 2012
Figure 3. Geologic map of the Tama Kosi-Rolwaling Himalaya. The section depicted in Figure 4 is shown along the main river valley between lettered control points “A” through “H.”
Journal Article
Journal: Geosphere
Published: 01 April 2012
Geosphere (2012) 8 (2): 507–517.
...Figure 4. Vertical geologic section along the Tama Kosi River. Approximate distribution of metamorphic index minerals is shown. See Figure 3 for lithologic legend. Dashed lines indicate interpreted eroded unit contacts. Dotted lines indicate interpreted structural fabric orientation. ...
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Journal Article
Published: 01 December 1968
Bulletin of Canadian Petroleum Geology (1968) 16 (4): 431–445.
... of limestone correlated with the Middle Devonian Abitibi River Formation. Overlying strata are 23 ft of overburden referred to Pleistocene and Recent. INTRODUCTION The Kaskat tama No. I well, of f ic ia l ly named Sogepet -Aqu i ta ine -Kas - kat tama Prov ince No. 1, is on the west shore of the cent ra l...
Journal Article
Published: 15 November 2019
Journal of the Geological Society (2020) 177 (2): 343–356.
...Alexandra Tamas; Dan Mircea Tamas; Csaba Krezsek; Zsolt Schleder; Giuseppe Palladino; Razvan Bercea Abstract Sand intrusions are commonly associated with hydrocarbon-bearing clastic reservoirs and they can host a significant part of the reserves. They modify the depositional sandbody architecture...
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Journal Article
Published: 01 April 2011
Bulletin of the Seismological Society of America (2011) 101 (2): 826–847.
... representation of the Tamar Valley. Arrays of radii 50 m and 100 m are presented for sites TamA( x =-100 m) and TamB( x =100 m). Solid vertical lines, edges of the valley ( x =-350 m, x =350 m); dashed vertical line, the axis of the valley at its deepest point ( x =-100 m). An analytical expression...
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Journal Article
Journal: Geosphere
Published: 01 April 2014
Geosphere (2014) 10 (2): 292–307.
... only one large-scale thrust fault, the Main Central thrust, through the region. Moreover, a recent examination of the Tama Kosi region, the next major drainage to the west of the Likhu Khola, concluded that neither the interpretation of Ishida (1969) nor Schelling (1992) was applicable...
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Journal Article
Published: 01 March 2006
Journal of Paleontology (2006) 80 (2): 367–379.
.... Kikuchi , T. 1991 . Geology of the Tama River bed, from which the tusk of Stegodon aurorae was recovered [Tamagawa kasho, Akebonozou Sesshi kaseki sanshutsuchi no Chishitsu] . Bulletin of the Hinocity Furusato Museum , 1 : 25 – 42 ( In Japanese ). Kimura , M. 1992 . The Study...
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Journal Article
Published: 01 June 2008
Bulletin of the Seismological Society of America (2008) 98 (3): 1429–1446.
... vicinity, increases to 60 m to the east of the fault, and reaches 80 m around the deepest parts of the Nanakita and Natori rivers. In the north, Tertiary or pre-Tertiary rocks are outcropping. Note that slopes of the Quaternary layers are very small, except at the Nagamachi–Rifu fault, as indicated...
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Journal Article
Journal: Geophysics
Published: 22 December 2010
Geophysics (2010) 75 (6): WB1–WB2.
...Sergey Fomel; Tamas Nemeth; Mauricio Sacchi Abstract Seismic data processing and imaging is concerned with the reconstruction of the subsurface image of the earth from measured seismic data. The quality of the reconstruction is highly dependent on the quantity and quality of the acquired seismic...
Journal Article
Published: 27 April 2023
Journal of the Geological Society (2023) 180 (3): jgs2022-148.
... settings to better understand the stratigraphic, sedimentological and structural character of potential or actual reservoir units in the subsurface (e.g. Tamas et al. 2022 ). These rocks are typically deemed to be equivalent based on similarities in their age, proximity or geological character...
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Journal Article
Published: 01 December 1969
Bulletin of Canadian Petroleum Geology (1969) 17 (4): 370–375.
... Bay in the central Hudson Bay Lowlands about 5 m i north of the mouth of the Kaskattama River (Fig . 1) . Drilled inter- mittently from September 1966 to July 1967, this well penetrated 291 3 ft of Phanerozoic strata and bottomed at 2941 ft in Precambrian base - ment. The well is important both...
Journal Article
Published: 01 February 1993
Bulletin of the Seismological Society of America (1993) 83 (1): 64–84.
... cross the relatively competent Pleistocene age sediments to the south of the Tama River, which could speed the wave up considerably. The phase that fits the Fuchu well log-derived dispersion curve best is the late arrival from the E. Yamanashi mainshock. Initially, we believed that the pair of scattered...
Journal Article
Published: 01 December 1995
Bulletin of the Seismological Society of America (1995) 85 (6): 1770–1789.
... eslee and Malin (1991) evaluated frequency-independent Q at the line, increases to 60 m to the east, and reaches 80 m from decay rates of spectral ratios between surface and bore- around the deepest part of the Nanakita River. In the north, hole records at a depth of about 200 m at two sites in Cali...