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Taz River

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Journal Article
Published: 01 April 2014
Russ. Geol. Geophys. (2014) 55 (4): 483–494.
...V.S. Volkova Abstract The paper is concerned with the structure of the Arctic shelf sediments in the Ob’ region in the Paleogene and Neogene, sampled from boreholes drilled on the Yamal Peninsula, in the lower reaches of the Pur and Taz Rivers. The specifics of Paleogene marine sedimentation...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1963
AAPG Bulletin (1963) 47 (7): 1294–1347.
... was made north of the Arctic Circle in the valley of the Taz River. Another large gas find was made in southern Uzbekistan. 1 Manuscript received, April 10, 1963. 2 American Overseas Petroleum Limited. © 1963 American Association of Petroleum Geologists. All rights reserved 1963...
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River-sea profiles across the marginal filters of the Yenisei and Ob’-Pur-Taz Rivers in the Kara Sea (the Dmitry Mendeleev research vessel voyage in August-October, 1993) [176]. A full set of oceanological investigations was performed at all stations. Sedimentation traps were used for the first time to study sediment flows, quantitative distribution and composition of suspension, colloidal and biological activity in marginal filters, and sedimentation rate. The Baidarata profile characterizes a weak influence of river water – the processes outside the area of avalanche sedimentation. 1 – stations with long-exposed sedimentation traps; 2 – stations with short-exposed sedimentation traps or with traps lost during storms.
Published: 01 April 2001
Fig. 8. River-sea profiles across the marginal filters of the Yenisei and Ob’-Pur-Taz Rivers in the Kara Sea (the Dmitry Mendeleev research vessel voyage in August-October, 1993) [ 176 ]. A full set of oceanological investigations was performed at all stations. Sedimentation traps were used
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Areal boundaries of the Sanchugovka-Salemal sea and the Taz glaciation. 1 –Sanchugovka-Salemal paleobasin, marine sediments; 2 – southern boundary of the transgression; 3 – gulfs and deltas; 4 – river valleys, alluvial, mainly sandy deposits; 5 – the bound of the maximum expansion of the Taz glaciation; 6 – sections in which marine beds contain benthic or, less frequently, planktonic foraminifers; 7 – the same, with remains of plankton species; 8 – the same, without foraminifers.
Published: 01 June 1998
Fig. 8. Areal boundaries of the Sanchugovka-Salemal sea and the Taz glaciation. 1 –Sanchugovka-Salemal paleobasin, marine sediments; 2 – southern boundary of the transgression; 3 – gulfs and deltas; 4 – river valleys, alluvial, mainly sandy deposits; 5 – the bound of the maximum
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Geological profile along the Yenisei River. Correlation between the Sanchugovka marine beds and the Taz and Samarovo moraines in the stratigraphic range between the Turukhan and Kazantsevo Horizons. 1 – boulders and pebbles in a sand-loamy matrix, the horizon oferosion of the underlying Samarovo moraine; 2 – TL dates (ka). Deposit indices: blg – Bolgokhtokh, nz – Nizyamy; tr – Turukhan; tz(sn2) – Taz (upper member of the Sanchugovka Formation). Other designations follow Figs. 1 and 3.
Published: 01 June 1998
Fig. 6. Geological profile along the Yenisei River. Correlation between the Sanchugovka marine beds and the Taz and Samarovo moraines in the stratigraphic range between the Turukhan and Kazantsevo Horizons. 1 – boulders and pebbles in a sand-loamy matrix, the horizon oferosion of the underlying
Journal Article
Published: 01 August 1999
Russ. Geol. Geophys. (1999) 40 (8): 1103–1116.
.... Deposits with similar associations were exposed by BH-38 in the center of the Taz Peninsula at depths of 194–150 m below the Ob’ River level. Pollen is unevenly distributed in the sediments. One half of the sequence contains occasional spores and pollen grains. The other half contains notable amounts...
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Stratigraphic location of the Taz moraine in the northern Ob’ region. Left bank of the Ob’ River, Salekhard key region [15]. 1 – clays; 2 – varved clays; 3 – silts, silty clays; 4 –loams; 5 – boulder loams; 6 – sands; 7 – sands alternating with clays and silts; 8 – sands with shingle partings; 9 – shingles; 10 – foraminifers. Deposit indices follow [15]: Q22sm – Samarovo; Q23slm – Salemal; Q24tz – Taz; Q31kz – Kazantsevo; Q32er – Ermakovo; Q33hr – Kharsoim; Q33lpg – Lokhpodgort; Q34sr – Sartan.
Published: 01 June 1998
Fig. 1. Stratigraphic location of the Taz moraine in the northern Ob’ region. Left bank of the Ob’ River, Salekhard key region [ 15 ]. 1 – clays; 2 – varved clays; 3 – silts, silty clays; 4 –loams; 5 – boulder loams; 6 – sands; 7 – sands alternating with clays and silts; 8 – sands
Journal Article
Published: 01 September 2018
Russ. Geol. Geophys. (2018) 59 (9): 1109–1119.
...F.I. Enikeev Abstract Paleogeographic reconstructions for the Samarovo, Taz, Murukta, and Sartan glaciations reveal the formation conditions of proglacial lakes dammed by ice in intermontane depressions and valleys of large rivers in eastern Transbaikalia. Middle–Late Pleistocene climate change...
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Journal Article
Journal: PALAIOS
Published: 01 May 2015
PALAIOS (2015) 30 (5): 388–402.
... in the Touro Passo River, dead shells are rapidly destroyed at the TAZ (also characterized by a subtropical climatic condition). Thus, the fossilization potential of the present-day shells in the Touro Passo River death assemblage was low or extremely improbable. Hence, those shells might have a low residence...
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Journal Article
Published: 01 December 1997
Russ. Geol. Geophys. (1997) 38 (12): 1891–1911.
... ( Figs. 1 and 2 ), the Kazantsevo marine deposits with the Kazantsevo complex of foraminifers are situated between the Taz and Ermakovo (Lower Zyrjanka) moraines, as it is established on the lower reaches of the Ob’ River, in the Salekhard reference terrain, as well as in the section of BH-4 drilled...
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Journal Article
Published: 01 June 2000
Russ. Geol. Geophys. (2000) 41 (6): 765–771.
... (Pustoe and Karapovskoe winter stations), and in northern Yamal [ 34 ]. The portland transgression did not reach the Yenisei valley. Its traces are absent from the entire territory from Taz River to Putorana Plateau. In the valley of the lower and middle Ob’, the upper stage appears as the Kolpashevo...
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Journal Article
Published: 01 June 1998
Russ. Geol. Geophys. (1998) 39 (6): 833–852.
...Fig. 8. Areal boundaries of the Sanchugovka-Salemal sea and the Taz glaciation. 1 –Sanchugovka-Salemal paleobasin, marine sediments; 2 – southern boundary of the transgression; 3 – gulfs and deltas; 4 – river valleys, alluvial, mainly sandy deposits; 5 – the bound of the maximum...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1972
AAPG Bulletin (1972) 56 (3): 454–471.
.... The Tobol’ River from the southwest and the Irtysh River from the south join the Ob’River from the southeast near the middle of the basin. The Ob’ flows northward along the west side of the basin to the Arctic Ocean. The northeast part is drained by the Pur and Taz Rivers. Some geologists believe the basin...
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Journal Article
Journal: PALAIOS
Published: 01 February 2004
PALAIOS (2004) 19 (1): 39–50.
... characteristics relative to residence times within the TAZ and above the DFB. Note that contours of all plots except skewness (D and G) are logarithmic. Dashed lines represent depression contours. Shaded areas indicate the extreme values of standard deviation and skewness for shell ages from Colorado River Delta...
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Journal Article
Journal: Paleobiology
Published: 01 August 2024
Paleobiology (2024) 50 (3): 424–451.
... in the subsurface SZ is one long-suspected means of increasing the persistence of shells exhumed back to the TAZ through Ostwald ripening (crystallite coarsening), mineral coatings, or micritization both in siliciclastic and carbonate environments (Jenkyns 1975 ; Kidwell 1989 ; Reid et al. 1990 ; Rivers et al...
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Journal Article
Journal: Paleobiology
Published: 01 August 2023
Paleobiology (2023) 49 (3): 527–562.
..., or incompletely mixed layer (IML; Guinasso and Schink 1975 ; Schiffelbein 1986 ; Savrda and Bottjer 1989 ; Soetaert et al. 1996 ; Ridgwell 2007 ; Tomašových et al. 2019b ). Tomašových et al. ( 2014 ) modeled the sequestration rate (τ) at which shells transition from a TAZ with high...
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FIGURE 6—Maps of shell age distribution characteristics relative to residence times within the TAZ and above the DFB. Note that contours of all plots except skewness (D and G) are logarithmic. Dashed lines represent depression contours. Shaded areas indicate the extreme values of standard deviation and skewness for shell ages from Colorado River Delta cheniers (Table 1). (A) Percentage of shells passing below DFB (i.e., entering the fossil record). (B) Locally averaged mean shell age. (C) Locally averaged standard deviation of shell age. (D) Locally averaged skewness of shell age. (E) Areally averaged mean shell age. (F) Areally averaged standard deviation of shell age, (G) Areally averaged skewness of shell age
Published: 01 February 2004
FIGURE 6 —Maps of shell age distribution characteristics relative to residence times within the TAZ and above the DFB. Note that contours of all plots except skewness (D and G) are logarithmic. Dashed lines represent depression contours. Shaded areas indicate the extreme values of standard
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Sanchugovka Formation in the stratotype (Sanchugovka River), parastrato-type in the Nikitinskii Gill (A), and key borehole 7B (Bolgokhtokh) (B). 1 – clays, silty clays, and silts, interbeds with scattered detritus; 2 – boulder sandy loams, in places boulder sands; 3 – boulder-shingle (residual moraine); 4a – shells of marine mol-lusks; 4b – the same, redeposited; 5a – foraminifers; 5b – the same, redeposited. Deposit indices: mes – Messo Formation according to Saks [1, 2], sm – Samarovo moraine; sn1 – lower member of the Sanchugovka Formation;sn2 – upper (Taz) member of the same formation; kz – Kazantsevo; nk(kz) – Nikitinskii deposits; sr –Sartan deposits. Designations in the inset: 1 – stratotype of the Sanchugovka Formation; 2 – parastratotype; 3 – Nikitinskii Gill.
Published: 01 June 1998
Fig. 3. Sanchugovka Formation in the stratotype (Sanchugovka River), parastrato-type in the Nikitinskii Gill ( A ), and key borehole 7B (Bolgokhtokh) ( B ). 1 – clays, silty clays, and silts, interbeds with scattered detritus; 2 – boulder sandy loams, in places boulder sands; 3 – boulder
Journal Article
Published: 01 June 1997
Russ. Geol. Geophys. (1997) 38 (6): 1086–1091.
... lower reaches of the Ob’ and Yenisei Rivers. The main glacier features are the Ob’, Polui, Nadym, Pur, Taz, and Yenisei lobes ( Fig. 4 ). The orientation of glaciodepressions and bands of marginal glacier formations, outlining them in an arch-like fashion from the south, indicates that within three...
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Journal Article
Published: 22 October 2024
Journal of Foraminiferal Research (2024) 54 (4): 375–393.
... molluscs from the Taphonomically Active Zone (TAZ) in marine core SV#23, Gulf St. Vincent. The results of some earlier gas chromatography analyses are also reported in this work relating to a marine vibracore from southern Gulf St. Vincent, southern South Australia (next section). The analytical...
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