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Kimin Formation

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Studied ambers.  A ) Amber embedded in a mudstone (black arrow) along with ...
in > PALAIOS
Published: 15 May 2018
Fig. 1.— Studied ambers. A ) Amber embedded in a mudstone (black arrow) along with Dipterocarpaceae leaf impression, Kimin Formation, Siwalik Group. B ) Amber embedded in a shale mudstone, Kimin Formation, Siwalik Group.
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(A) Geological map of the study area. (B–C) Schematic stratigraphic logs of...
Published: 01 March 2013
, corresponding locally to the Dafla, Subansiri, and Kimin Formations. Abbreviations: s—silt, vf—very fine sand, f—fine sand, m—medium sand, c—coarse sand, vc—very coarse sand. Paleocurrent directions are indicated where they could be measured.
Journal Article
Journal: PALAIOS
Published: 15 May 2018
PALAIOS (2018) 33 (5): 218–227.
...Fig. 1.— Studied ambers. A ) Amber embedded in a mudstone (black arrow) along with Dipterocarpaceae leaf impression, Kimin Formation, Siwalik Group. B ) Amber embedded in a shale mudstone, Kimin Formation, Siwalik Group. ...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2010
GSA Bulletin (2010) 122 (3-4): 360–395.
... Gondwana Sequence over Tertiary strata, and the Tipi thrust places the Miocene Dafla Formation over the Pliocene Subansiri and Pleistocene Kimin Formations ( Kumar, 1997 ). The Main Frontal thrust zone consists of a series of en echelon folds that branch off obliquely from the main Himalayan Range front...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2013
GSA Bulletin (2013) 125 (3-4): 523–538.
..., corresponding locally to the Dafla, Subansiri, and Kimin Formations. Abbreviations: s—silt, vf—very fine sand, f—fine sand, m—medium sand, c—coarse sand, vc—very coarse sand. Paleocurrent directions are indicated where they could be measured. ...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2013
GSA Bulletin (2013) 125 (3-4): 499–522.
... in the Jaishidanda Formation, quartzite and phyllite in the Daling-Shumar Group, quartzite and minor carbonates in the Baxa Formation, and sandstones and shales of the Gondwanan succession ( Gansser, 1983 ; Bhargava, 1995 ; McQuarrie et al., 2008 ). Detrital zircon U-Pb geochronology yields maximum depositional...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2012
GSA Bulletin (2012) 124 (9-10): 1449–1473.
... samples, a unique zircon population from the Gonggar sample site, defined by the Gonggar domain in Figure 5F , overlaps the data points from sandstone samples of the Dafla and Subansiri Formations in the eastern Himalayan foreland. Modal composition of the Men Qu sample (DJG0803; site 1 in Fig...
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Series: Geological Society, London, Special Publications
Published: 25 September 2019
DOI: 10.1144/SP481.7
EISBN: 9781786204264
... to Taliha in the north ( S. Kumar & Singh 1980 ; G. Kumar 1997 ; Yin et al. 2010 ) ( Fig. 1a, b ). The Sub-Himalaya is represented by the Kimin Formation, which has a thrust contact with the Brahmaputra alluvium in the south and the Lesser Himalaya in the north along the Himalayan Frontal Thrust...
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Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2404(10)
... is thinnest and the total contributing area is greatest, than in the interior, where the rate of mixing-driven dissolution may be below the critical limit for cave formation. Support is provided for this suggestion by the coupled geochemical and hydrological modeling study of Sanford and Konikow (1989...
Journal Article
Journal: GSA Bulletin
Published: 01 September 2016
GSA Bulletin (2016) 128 (9-10): 1403–1422.
... these units are locally called the Kimin, Subansiri, and Dafla formations ( Kumar, 1997 ), we adopt the corresponding Upper, Middle, and Lower Siwalik Formation nomenclature for consistency with the well-established, broader Himalayan literature (e.g., Pilgrim, 1913 ) and previous work from the same location...
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