Paleoclimate and paleovegetation of Lower Narmada Basin, Gujarat, Western India, inferred from stable carbon and oxygen isotopes

AH Laskar, N Sharma, R Ramesh, RA Jani… - Quaternary …, 2010 - Elsevier
Surface sediment samples (depth 0–160cm) and a paleosol (depth 10–15m), both part of a
sediment profile exposed in a cliff section of Narmada River, Western India were analyzed …
被引用次数：25 相关文章

[引用][C] Paleoclimate and paleovegetation of Lower Narmada Basin, Gujarat, Western India, inferred from stable carbon and oxygen isotopes

AH Laskar, N Sharma, R Ramesh… - Quaternary …, 2010 - ui.adsabs.harvard.edu
Paleoclimate and paleovegetation of Lower Narmada Basin, Gujarat, Western India,
inferred from stable carbon and oxygen isotopes - NASA/ADS Now on home page ads icon …

Paleoclimate and paleovegetation of Lower Narmada Basin, Gujarat, Western India, inferred from stable carbon and oxygen isotopes

AH Laskar, N Sharma, R Ramesh, RA Jani… - Quaternary …, 2010 - infona.pl
Surface sediment samples (depth 0–160cm) and a paleosol (depth 10–15m), both part of a
sediment profile exposed in a cliff section of Narmada River, Western India were analyzed …
[PDF] academia.edu

[PDF][PDF] Paleoclimate and paleovegetation of Lower Narmada Basin, Gujarat, Western India, inferred from stable carbon and oxygen isotopes

AH Laskar, N Sharma, R Ramesh, RA Jani… - Quaternary …, 2010 - academia.edu
abstract Surface sediment samples (depth 0e160 cm) and a paleosol (depth 10e15 m), both
part of a sediment profile exposed in a cliff section of Narmada River, Western India were …

Paleoclimate and paleovegetation of Lower Narmada Basin, Gujarat, Western India, inferred from stable carbon and oxygen isotopes

AH Laskar, N Sharma, R Ramesh, RA Jani… - Quaternary …, 2010 - repository.ias.ac.in
Surface sediment samples (depth 0-160 cm) and a paleosol (depth 10-15 m), both part of a
sediment profile exposed in a cliff section of Narmada River, Western India were analyzed …

Paleoclimate and paleovegetation of Lower Narmada Basin, Gujarat, Western India, inferred from stable carbon and oxygen isotopes

AH Laskar, N Sharma, R Ramesh, RA Jani… - Quaternary …, 2010 - repository.ias.ac.in
Surface sediment samples (depth 0-160 cm) and a paleosol (depth 10-15 m), both part of a
sediment profile exposed in a cliff section of Narmada River, Western India were analyzed …
[PDF] academia.edu

[PDF][PDF] Paleoclimate and paleovegetation of Lower Narmada Basin, Gujarat, Western India, inferred from stable carbon and oxygen isotopes

AH Laskar, N Sharma, R Ramesh, RA Jani… - Quaternary …, 2010 - academia.edu
abstract Surface sediment samples (depth 0e160 cm) and a paleosol (depth 10e15 m), both
part of a sediment profile exposed in a cliff section of Narmada River, Western India were …

[引用][C] Paleoclimate and paleovegetation of Lower Narmada Basin, Gujarat, Western India, inferred from stable carbon and oxygen isotopes

AH LASKAR, N SHARMA, R RAMESH, RA JANI… - Quaternary …, 2010 - Elsevier