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Markha River basin

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... Abstract Stratigraphic analysis of sedimentary basins is critical for correlation in a basin, for reconstructing the geohistory of a basin, and for developing a successful petroleum exploration strategy for a basin. In studying only the shelfal areas of basins that are characterized...
Journal Article
Published: 01 October 2019
Russ. Geol. Geophys. (2019) 60 (10): 1175–1187.
... of these bitumens, provides a compelling evidence of their consanguinity. The bitumen and oil of kimberlite pipes in the south of the basin, in the area of reefs of the Siligir–Markha bar, are similar in all geochemical criteria to oils of the Nepa–Botuobiya anteclise. In particular, in primary geochemical...
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Journal Article
Published: 01 May 2013
Russ. Geol. Geophys. (2013) 54 (5): 555–565.
..., in the eastern margin of the Tunguska basin (Siberian craton). It is an area of hilly topography, with watersheds at 400–440 m and river tables at 100–150 m above sealevel (asl). The water table of the Markha River in the PUNE vicinity is about 290 asl. The Ediacaran sediments are dolimites and stromatolitic...
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Journal Article
Published: 01 October 2018
Russ. Geol. Geophys. (2018) 59 (10): 1204–1216.
..., ° Λ, ° dm/dp , ° fm , ° Reference φ, ° λ, ° I. Angara–Anabar terrane Irkutsk basin 1 Variegated silty sandstones of the Vendian Khuzhir Fm. Vhz, Irkut River 52.1 103.8 10/– 207.3 2.3 13.3 13.8 –32 71 6.9/13.8 1 Kravchinsky et al., 2001 Vilyui-Markha dike swarm...
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Journal Article
Published: 01 September 2008
Russ. Geol. Geophys. (2008) 49 (9): 655–666.
... Pyrope-almandine garnets lower crust kimberlite shield Siberian Platform The study area is located in the eastern Siberian Platform, on the northwestern margin of the Vilyui syneclise, and is bounded by the Muna and Markha Rivers ( Fig. 1 ). Geographically, it is the eastern margin...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2017
GSA Bulletin (2017) 129 (7-8): 820–836.
... from the western Himalaya into the Arabian Sea for roughly the last ∼45 m.y. ( Clift et al., 2001 ). The broader Zanskar River basin can be subdivided into the five catchments of the main tributaries: the Tsarap, Stod, Khurna, Markha, and Oma Rivers ( Fig. 1C ). Glaciers occupy 8% of the Zanskar...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2017
GSA Bulletin (2017) 129 (1-2): 203–217.
... and the distribution of erosion and transported sediment to surrounding sedimentary basins. Any modification of catchment shape also has implications for the scaling of upstream catchment area with channel length and hence the long profile of rivers ( Whipple and Tucker, 1999 ; Willett et al., 2014 ). Fluvial...
Journal Article
Published: 01 November 2014
Russ. Geol. Geophys. (2014) 55 (11): 1316–1320.
.... The first one was discovered by K.K. Makarov in the field of Middle Cambrian sediments in the basin of the upper stream of the Olenek River (Arga-Sala River area), on the southern slope of the Anabar anteclise, in the 1960s (Makarov and Kosolapov, 1967). Makarov associated this oil show with the oil pool...
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Journal Article
Published: 01 February 2013
Russ. Geol. Geophys. (2013) 54 (2): 121–137.
... are overlain by sheets of the Middle Carboniferous–Cretaceous sediments of the Vilyui syneclise, which are >6 km thick in the axial part. In the northwest and southeast, the Vilyui basin is bounded by two dike swarms: Vilyui–Markha and Chara–Sinyaya, respectively. The dolerite body (sample from a borehole...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2011
GeoArabia (2011) 16 (1): 113–134.
... ). The northern and southern provinces are characterized by regional SW dip, whereas the central province by regional NE dip. On a more detailed scale, the Gulf can be divided into smaller sub-basins or half-grabens ( Hagras, 1986 ; Farhoud, 2009). The present study is focused on two half-grabens located west...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2014
GSA Bulletin (2014) 126 (11-12): 1580–1594.
... appreciated comments by Sarah Penniston-Dorland, Craig Dietsch, and an anonymous reviewer, and thank Christian Köberl for handling the manuscript. REFERENCES CITED Ali K.F. de Boer D.H. , 2007 , Spatial patterns and variation of suspended sediment yield in the upper Indus River basin...
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Journal Article
Published: 01 October 2018
Russ. Geol. Geophys. (2018) 59 (10): 1217–1236.
... 1. 40 Ar/ 39 Ar ages of dikes of the Yakutsk–Vilyui Large Igneous Province Sample no., source Age, Ma Rock Location Coordinates Dike swarm A-84-67, ( Polyansky et al., 2017 ) 389.7 ± 3.6 Gabbro-dolerite Dike A-84, Tyung–Muna Rivers interfluve 67°03′ N, 117°27′ E Vilyui–Markha...
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Journal Article
Published: 01 February 2018
Russ. Geol. Geophys. (2018) 59 (2): 144–156.
... ground ices with the river waters of the permafrost zone (Sytykan River basin, Daldyn–Alakit region) and with the groundwater of the hypergenesis segment of this zone showed higher contents of trace components, except for Sc, Cr, and Hf ( Table 3 ). The enrichment or depletion of ground ice in trace...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2010
GeoArabia (2010) 15 (2): 175–204.
...Moujahed I. Al-Husseini; M. Dia Mahmoud; Robley K. Matthews ABSTRACT The Miocene Kareem Formation in the Egyptian Gulf of Suez, and its equivalent formations throughout the Red Sea (250–550 m thick), contain one of the most important petroleum reservoirs in these highly faulted rift basins...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP282.15
EISBN: 9781862395305
... (e.g. rift; accretionary prism; foreland basin) have been identified and termed tectonic facies ( Robertson 1994 ). In mountain belts generally the proximal (inboard) parts of rifted continental margins are formed on relatively thick continental crust and these are commonly well preserved...
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Journal Article
Published: 01 April 2013
Russ. Geol. Geophys. (2013) 54 (4): 357–380.
..., and for the conditions of rifting (extension), in the case of the Vilyui basin. As the modeling shows, formation of a superdeep basin does not necessarily require the crust to stretch twice or more: only 20% stretching in the necking region is enough to produce a 10–15 km deep basin. strain stress subduction...
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Journal Article
Published: 01 May 2009
Russ. Geol. Geophys. (2009) 50 (5): 417–429.
... (traceable along the Yangeto River, a right tributary of the Vivi River, which, in turn, is a right tributary of the Nizhnyaya Tunguska River) does not have a single representative stratotype either. In contrast to the stratotype section in the Yangeto basin (sandstones with gravelstone lenses and rare...
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Journal Article
Published: 01 March 2007
Russ. Geol. Geophys. (2007) 48 (3): 225–236.
... of the Tunguska, Angara-Lena, western part of the Yakutian and Olenek artesian basins and 87 Sr/ 86 Sr in brines of the western part of the Olenek artesian basin was studied in the context of the problem of genesis of highly mineralized groundwaters. Results of the study and comparative analysis...
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Journal Article
Published: 01 March 2002
Geological Magazine (2002) 139 (2): 159–169.
...SERGEI B. FELITSYN; ALEXANDER P. GUBANOV Abstract A Nd isotope map of early Cambrian epeiric basins has been inferred from the Nd isotopic signature recorded in phosphatic Small Shelly Fossils. The most radiogenic ε Nd (t) values characterize water reservoirs along the Avalonian and Cadomian belts...
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Journal Article
Published: 01 July 2021
Russ. Geol. Geophys. (2021) 62 (07): 746–764.
.... Kobayashi from I.P. Tolmachev’s collection. Their location was established as the Giranda River (original spelling) of the Khatanga-Anabar Basin, (ibid., p. 288). It was noted in V. E. Savitskii’s study on the southwestern slope of the Anabar uplift that Tolmachev’s collection from 1905–1907, published...
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