Waseem Raza
Biographic Data
| ID | 7483816 |
|---|---|
| NAME | Waseem Raza |
| GIVEN NAMES | Waseem |
| FAMILY NAME | Raza |
| SIGNATURE | RAZA W |
| AFFILIATIONS | National Geophysical Research Institute |
| ORCID | 0000-0003-0429-8628 |
| VERIFIED | Yes |
| TOTAL WORKS | 6 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 6 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2011 |
| LATEST PUBLICATION YEAR | 2024 |
| H-INDEX | 0 |
Geochemistry and Mineralogy of Peninsular Indian River Sediments with Special Reference to Godavari and Krishna Rivers
Response of trace and rare earth elements to environmental changes in a stalagmite from southern India for the last deglaciation
Speleothems, particularly stalagmites are extensively used to reconstruct paleoclimatic and paleomonsoon changes by using stable oxygen and carbon isotopes along the growth profile of a stalagmite sample. Trace and rare earth elements (REEs) variations in stalagmites are widely recognized as indicators of past precipitation and local hydrology. The amalgamation of isotopic and trace element proxies in speleothems has been regarded as an important…
Stalagmite based high resolution precipitation variability for past four centuries in the Indian Central Himalaya
Oxygen isotopic evidence for decrease in calcification rate of Porites coral from the Lakshadweep Island
Climatic fluctuations during the LIA and post-LIA in the Kumaun Lesser Himalaya, India
High-resolution carbon and oxygen isotope records from a scleractinian (Porites) coral of Lakshadweep Archipelago
No prominent works on this page.
High-resolution carbon and oxygen isotope records from a scleractinian (Porites) coral of Lakshadweep Archipelago
Climatic fluctuations during the LIA and post-LIA in the Kumaun Lesser Himalaya, India
Oxygen isotopic evidence for decrease in calcification rate of Porites coral from the Lakshadweep Island
Stalagmite based high resolution precipitation variability for past four centuries in the Indian Central Himalaya
Response of trace and rare earth elements to environmental changes in a stalagmite from southern India for the last deglaciation
Speleothems, particularly stalagmites are extensively used to reconstruct paleoclimatic and paleomonsoon changes by using stable oxygen and carbon isotopes along the growth profile of a stalagmite sample. Trace and rare earth elements (REEs) variations in stalagmites are widely recognized as indicators of past precipitation and local hydrology. The amalgamation of isotopic and trace element proxies in speleothems has been regarded as an important…
Geochemistry and Mineralogy of Peninsular Indian River Sediments with Special Reference to Godavari and Krishna Rivers
Geology (5 works) · Climatology (4 works) · Monsoon (4 works) · Cave (3 works) · East Asian Monsoon (3 works) · Geography (3 works) · Geology and Paleoclimatology Research (3 works) · Holocene (3 works) · Oceanography (3 works) · Paleontology (3 works)