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Gaj River

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Journal Article
Published: 01 April 1974
Micropaleontology (1974) 20 (2): 178–193.
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1959
AAPG Bulletin (1959) 43 (11): 2675–2700.
... development from rivers rising in the high Himalayas. The shortage of power was a serious handicap to any efforts to expand industrial activity so that the discovery of the Sui gas field in 1952 was an event of great economic importance; the reserves were later proved to be 4–5 million million cubic feet...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1986
AAPG Bulletin (1986) 70 (6): 730–747.
...-Indian margin, superimposed by a terrigenous clastic depositional system comprised of deltas, shelves, and deep-sea fans of the Indus River. Aeromagnetic surveys of the Southern Indus basin were conducted by Standard Vacuum Oil Company (SVOC) in 1955, and by the OGDC in 1962-1963. Gravity surveys...
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Journal Article
Published: 01 July 2021
Journal of Paleontology (2021) 95 (4): 763–776.
..., 2014 ) showing the pleurotomariid-bearing horizons. The Dwarka Basin, situated at the western fringe of the Kathiawar Peninsula, is a peri-cratonic shelf basin, and filled with an extensive succession of marine sediments. The succession is subdivided into three formations—the Gaj, Dwarka...
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Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.195.01.15
EISBN: 9781862394438
..., in the Khude and Zarro Ranges (up to 800 m) and in the Laki Range and Gaj River area (up to 1000 m); also developed throughout M1B Unconformity above lower Pab in Laki Range, passing westward into a correlatable conformity above Mughal Kot in Pab Province Up to 400 m of gravelly Pab sandstone turbidites...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1934
AAPG Bulletin (1934) 18 (3): 283–314.
... and Upper Miocene), 5,000-11,000 feet Sandstones, conglomerates, and silty clays, divisible into formational units of variable persistence, on basis of lithology; most of area is designated on map as “later Tertiary” Gaj (Miocene), 0-1,500 feet Sandstones, shales and clays, interbedded with calcareous...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 2004
AAPG Bulletin (2004) 88 (7): 1007–1035.
... of Blanford, 1878 and Venericardia shales of Eams, 1952 ); Rakhi Gaj Formation (lower Rakhi Gaj shales and Gorge beds of Eams, 1952 ); Girdu Member (Gorge beds of Eams, 1952 ), Dunghan Formation (Dunghan limestone of Oldham, 1890 , Zinda Pir shales and Zinda Pir limestone, lower part, all combined...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1982
AAPG Bulletin (1982) 66 (7): 940–946.
..., between Murray Ridge and the hinge line; (2) the offshore Karachi trough platform in the middle between the hinge line and the Karachi shoreline; and (3) offshore Thar slope platform or Indus River deltaic area on the east. The hinge-line zone and the outer margin of the carbonate platform, where...
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Journal Article
Published: 01 August 2012
Bulletin of the Seismological Society of America (2012) 102 (4): 1810–1819.
... of the Indus River, along its tributaries in the Punjab, or its distributaries in Sindh and may have been subjected to amplification typical of sediments and water‐saturated sediments. During the Monsoon of the preceding year, the Indus flooded, and it is possible that water tables were higher than usual...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1969
AAPG Bulletin (1969) 53 (7): 1480–1499.
..., representing most of the late Tertiary. Vredenburg (1909) referred to it as the Makran system, which he subdivided into stages. Parkini Mudstone .—The type locality of this formation is Parkini Kaur, a tributary of Hingol River east of the study area. The name was introduced by Hunting (1961, p. 238...
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Journal Article
Journal: PALAIOS
Published: 21 March 2022
PALAIOS (2022) 37 (3): 73–87.
... such as one caused by tectonic uplift influences a variety of physical parameters (such as sedimentation rate, river influx, salinity, etc.) that can affect the diversity and morphology of shallow marine ecosystems ( Scavia et al. 2002 ; Bakun 2010 ; Gilbert et al. 2010 ; Keeling et al. 2010 ). Shallow...
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Journal Article
Published: 01 July 2001
Geological Magazine (2001) 138 (4): 397–405.
... of the overlying Miocene Manchar Formation ( Raza et al. 1984 ). The Early Miocene Gaj Formation was interpreted as the oldest geological record of the Indus delta ( Kazmi, 1984 ). However, recent investigations in the Katawaz Basin (eastern Makran, Fig. 2 ) have led to the description of the Palaeogene...
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Journal Article
Published: 01 July 2008
The Journal of Geology (2008) 116 (4): 331–353.
..., south central Tibet . Tectonics 24 : TC3001 , doi: 10.1029/2004TC001729 . Dorreen J. M. 1974 . The western Gaj River section, Pakistan, and the Cretaceous-Tertiary boundary . Micropaleontology 20 : 178 – 193 . Eames F. E. 1951 . A contribution to the study of the Eocene...
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Journal Article
Published: 08 October 2020
Journal of Sedimentary Research (2020) 90 (9): 980–1010.
... by dating of calcretes, which showed that the core covers almost the entire Cenozoic. Two megafans could be distinguished. The older, buried Olukonda Megafan stems from a mafic source rock, potentially the Kunene Intrusive Complex, and was deposited by a paleo–Kunene River towards the southeast and east...
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Journal Article
Published: 01 December 2002
Journal of Micropalaeontology (2002) 21 (2): 115–130.
... Ferns & lowland marsh (freshwater) Arecipites spp. – tropical peat marshes Baculatisporites comauensis – Osmundaceae; lowland marsh or river fern Cicatricosisporites dorogensis – Schizeaecea; Pteridophyte, semi-arid tropical lowland marsh Cicatricosisporites segmentatus...
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Series: AAPG Hedberg Series
Published: 01 January 2004
DOI: 10.1306/1025688H13112
EISBN: 9781629810461
... assigned a type III or a mixed type II/III kerogen. No direct measurement of Goru/Sembar source rock quality in the study area is available. To the west in the Mor Range and to the north in Gaj River, the measured potential of the source rock is less than 2% total organic carbon (TOC) ( Figure 1...
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Journal Article
Published: 01 January 2013
Reviews in Mineralogy and Geochemistry (2013) 75 (1): 7–46.
..., Khatanga, Siberia C MCo Gra, Cu, Fe, Tro, Wus  R2 Coal Mine 45, Kopeisk, Urals C CoF Gra, Tro  R3 Is River, Isovsky District, Urals I, To Pla Os, Pt, Iso, Tet, Cup, Mal, Fer, Gup, Xif  R4 Verkhneivinsk, Neiva River, Urals I Pla Os, Ru, Any  R5 Billeekh intrusion, Saha Rep...
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Journal Article
Published: 01 May 2016
Vadose Zone Journal (2016) 15 (5): vzj2015.09.0131.
... methods (e.g., cryogenic distillation) for determining soil-water δ 2 H and δ 18 O signatures ( Gaj et al., 2015 ; Gangi et al., 2015 ). Another exciting challenge of the coming years is to determine plant-root water-uptake profiles via online and nondestructive determination of soil water δ 2 H and δ 18...
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Series: Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/GSL.SP.2007.275.01.16
EISBN: 9781862395237
... ) and recently redefined and/or re-illustrated by Pronina-Nestell & Nestell ( 2001 ). The fauna was revised by Kotlyar et al. ( 2004 ). The Nikitin section The field section at Nikitin is upstream from the Malaya Laba River, tributary of the Kuban River (Figs 1 a, b & 2a). It is located...
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Journal Article
Published: 01 January 2012
Reviews in Mineralogy and Geochemistry (2012) 74 (1): 279–364.
..., and/or recirculation is confined due to restricted communication with other basins, as for instance the Red Sea and the Mediterranean. Conversely, salinity is lower where mixing and dilution with fresh water runoff from rivers or glaciers is more abundant, notably in more moderate and polar climate regions, but also...
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