...Fig. 2. Borehole 11, lower reaches of the Pur River. 1 , diatomites interbedded with diatomaceous shales; 2 , clays; 3 , diatomites; 4 , sands; 5 , clay loams; 6 , silts; 7 , gravel and pebbles; 8 , carbonized remnants; 9 , core sampling sites. The age of the formations in the figures...

... by one or more of the following: 1) salt solution, 2) erosion of underlying rocks creating drainage basins, and 3) tectonic subsidence in western areas, particularly over the Peace River Arch. Five major erosional drainage basins are delineated on the basal unconformity. The basin through Saskatchewan...

... controlled by the physicochemical conditions of their formation (Eh, pH, activities of constituent cations, P and T). These minerals are particularly widespread and spatially related to hydrothermal clay-mineral parageneses in the East Alligator River Uranium Field (EARUF) environment associated with uranium...

... from the KHR mountain fronts (i.e. Pat and Pur River). (2) V f = 2 V fw / [ ( E ld − E sc ) + ( E rd − E sc ) ] Where, V fw is width of the valley floor, E sc is elevation of the valley floor with respect...

... Pu field lysimeter experiments at the Savannah River Site showed anomalous distributions below the source, with significant upward migration above the source. A previously developed reactive transport model with an initial application of a steady downward velocity successfully simulated the below...

... 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...

... and Chham, on the right banks of the Nagen gad and the Bbagirathi rivers in the Garhwal Himalaya, Jain (1971) reports the 'Laluri formation' below the Chand pur formation. However, it appears, from his lithological description, that the' Laluri formation' is a variant of the Mandhali formation which also...

... upon the Upper Cretaceous sediment (near Kamenny Mys Village) at a depth of 200–340 m (BH-12RR, BH-12RG), gradually subsiding toward the Gulf of Ob’. In BH-1K, the Lower Paleocene is already in the range 375–500 m. In the lower reaches of the Pur River, the Lower Paleocene deposits are exposed...

.... 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...

...\{C_{\mathrm{Puo}}(z,t)\left[1{+}\frac{\mathrm{{\rho}}}{\mathrm{{\theta}}(z,t)}K_{\mathrm{do}}\right]\right\}}{{\partial}t}{=}{-}\frac{{\partial}\left[v(z,t)C_{\mathrm{Puo}}(z,t){-}D(z,t)\frac{{\partial}C_{\mathrm{Puo}}(z,t)}{{\partial}z}\right]}{{\partial}z}\\&&{+}k_{\mathrm{o}}C_{\mathrm{Pur...

... (Figure 9-1), and is sited at the confluence of the Khari and Pur Rivers. The main earthen embankment is 875 m in length, with a maximum section height of 27.6 m. Figure 9-16 shows the design cross-section for this conventionallyzoned earth darn, and also illustrates observed damages and distress...

... UIGGM, SIBERIAN BRANCH OF THE RAS 2005 UIGGM, SIBERIAN BRANCH OF THE RAS Biogeochemistry lichens environmental pollution radionuclides trace elements vertical and horizontal distribution West Siberia Lichen cover was sampled during the expedition works in the north (Pur...

... prospects are located far north of the industrially developed areas of the middle reaches of the Ob River. At the end of 1984, the number of prospects in the basin’s portfolio was only 3 times greater than the number of prospects annually drilled. A significant portion of these new prospects were targets...

... River, within the southern Krasnoleninsk megamonoclise and in the northern part of the basin, within the Medvezh’ye-Numga tilted megaswell. The Br concentration near the framing is usually less than 10 mg/l. Fig. 5. Schematic map of bromine contents (mg/l) in underground waters of the West...

... another in the direction from the west to the east ( Fig. 1 ). The maxima here correlate with the Nadym megadepression (>120 °C) and Middle Pur trench (>110 °C), while the minima—with the most elevated parts of the Northern arch and Vyngapur swell (85–90 °C). Relatively low temperatures (74–80 °C...

... SettingLodai 2 Banni Plain N54~ Banni Plain N60-80~ Chang River Alluvial Plain 23.35795 69.69386 Lateral spread 350, >40, 0.8 v Sand blows 2.5, 2.3, 0.08 N25~ N15~ Reservoir on Pur River 23.20000 70.73333 Sand blows Little Rann 23.28333 70.00500 Sand blows Little Rann 23.24000 70.76000 Lateral spread SW Little...

..., A2 — Sidorovo-Suzun monocline, A3 — Krasnosel’kup inlier, A4 — Mid-Taz megatrough, A5 — Tol’ka elongate megaswell, A6 — Khadyr’yakh monocline, A7 — Lower-Pur elongate megaswell, A8 — Medvezhy elongate megaswell, A9 — Neruta megadepression, A10 — Tanlov elongate megaswell, A11 — Mid-Pur megatrough...