Jayant K Tripathi
Biographic Data
| ID | 7512632 |
|---|---|
| NAME | Jayant K Tripathi |
| GIVEN NAMES | Jayant K |
| FAMILY NAME | Tripathi |
| SIGNATURE | TRIPATHI J K |
| AFFILIATIONS | Jawaharlal Nehru University |
| VERIFIED | No |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2007 |
| LATEST PUBLICATION YEAR | 2015 |
| H-INDEX | 0 |
Late Holocene flooding history of a tropical river in western India in response to southwest monsoon fluctuations
Early holocene monsoonal fluctuations in the Garhwal higher Himalaya as inferred from multi-proxy data from the Malari paleolake
A 4.9-m-thick lake sequence, formed due to the landslide damming of a stream in the semiarid Garhwal Himalaya, was studied to understand past monsoonal variations in the region. The Optically Stimulated Luminescence (OSL) chronology indicates that the lake existed between ~ 12 and ~ 7 ka ago. Chronologically constrained trends of sand percent, organic phosphorus (OP), apatite inorganic phosphorus (AIP) and parameters of environmental magnetism we…
Fashion and phases of late Pleistocene aggradation and incision in the Alaknanda River Valley, western Himalaya, India
We study the aggradation and incision of the Alaknanda River Valley during the late Pleistocene and Holocene. The morphostratigraphy in the river valley at Deoprayag shows the active riverbed, a cut terrace, and a fill terrace. The sedimentary fabric of the fill terrace comprises four lithofacies representing 1) riverbed accretion, 2) locally derived debris fan, 3) the deposits of waning floods and 4) palaeoflood records. The sedimentation style,…
Geochemistry of sediments of the Ganges alluvial plains
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Geochemistry of sediments of the Ganges alluvial plains
Fashion and phases of late Pleistocene aggradation and incision in the Alaknanda River Valley, western Himalaya, India
We study the aggradation and incision of the Alaknanda River Valley during the late Pleistocene and Holocene. The morphostratigraphy in the river valley at Deoprayag shows the active riverbed, a cut terrace, and a fill terrace. The sedimentary fabric of the fill terrace comprises four lithofacies representing 1) riverbed accretion, 2) locally derived debris fan, 3) the deposits of waning floods and 4) palaeoflood records. The sedimentation style,…
Early holocene monsoonal fluctuations in the Garhwal higher Himalaya as inferred from multi-proxy data from the Malari paleolake
A 4.9-m-thick lake sequence, formed due to the landslide damming of a stream in the semiarid Garhwal Himalaya, was studied to understand past monsoonal variations in the region. The Optically Stimulated Luminescence (OSL) chronology indicates that the lake existed between ~ 12 and ~ 7 ka ago. Chronologically constrained trends of sand percent, organic phosphorus (OP), apatite inorganic phosphorus (AIP) and parameters of environmental magnetism we…
Late Holocene flooding history of a tropical river in western India in response to southwest monsoon fluctuations
Geology and Paleoclimatology Research (4 works) · Fluvial (3 works) · Geomorphology (3 works) · Holocene (3 works) · earthquake and tectonic studies (2 works) · Geochemistry (2 works) · Geography (2 works) · Geological and Geochemical Analysis (2 works) · Geological formations and processes (2 works) · Geology (2 works)