High resolution facies record on late Holocene flood plain sediments from lower reaches of Narmada Valley, Western India

被引：7

作者：

Sukumaran, Prabhin ^{[1
,3
]}

Sant, Dhananjay A. ^{[1
]}

Krishnan, K. ^{[2
]}

Rangarajan, Govindan ^{[4
]}

机构：

[1] Maharaja Sayajirao Univ Baroda, Fac Sci, Dept Geol, Vadodara 390002, Gujarat, India

[2] Maharaja Sayajirao Univ Baroda, Fac Arts, Dept Archaeol & Ancient Hist, Vadodara 390002, Gujarat, India

[3] Inst Seismol Res, Gandhinagar 382009, India

[4] Indian Inst Sci, Dept Math, Bangalore 560012, Karnataka, India

来源：

JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA | 2012年 / 79卷 / 01期

关键词：

Lower reaches of Narmada valley; Late Holocene; Sedimentology; Sediment facies; Hydrology; GRAIN-SIZE DISTRIBUTIONS; CLIMATE-CHANGE; STATISTICAL PARAMETERS; RIVER-BASIN; EVOLUTION; DEPOSITS; SYSTEM;

D O I：

10.1007/s12594-012-0009-z

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

A high resolution quantitative granulometric record for site Uchediya [21A degrees 43'2.22aEuro(3) N, 73A degrees 6'26.22aEuro(3) E; 10 m a. s. l.] gives understanding towards accretion history of the late Holocene flood plain in the lower reaches of Narmada River. Two sediment facies (sandy and muddy) and seven subfacies (sandy subfacies: St(MS+FS+CS), SmFS+MS, Sl(FS+VFS), and St(MS + CS); muddy subfacies: FmSILT+VFS+FS, FmSILT+VFS (O) and FmSILT+VFS (T)) are identified based on cluster analysis supplemented with sedimentary structures observed in field and other laboratory data. Changes in hydrodynamics are further deduced based on various sedimentological parameters and their ratios leading to arrive at a depositional model.

引用

页码：41 / 52

页数：12

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