Neven Bočić
Biographic Data
| ID | 6572422 |
|---|---|
| NAME | Neven Bočić |
| GIVEN NAMES | Neven |
| FAMILY NAME | Bočić |
| SIGNATURE | BOČIĆ N |
| AFFILIATIONS | University of Zagreb |
| ORCID | 0000-0001-6102-5330 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 1 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2018 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 1 |
Late Pleistocene - Holocene geomorphologic evolution of the Kvarner area (northern Adriatic, Croatia)
Holocene hydroclimate changes in continental Croatia recorded in speleothem δ 13 C and δ 18 O from Nova Grgosova Cave
We present the first stable isotope (δ 13 C and δ 18 O) speleothem record from continental Croatia retrieved from two coeval stalagmites from Nova Grgosova Cave. U-Th dates constrain the stalagmite growth history from 10 ka to the present, revealing coeval growth between 7.8 and 5.6 ka. We interpret δ 18 O as an autumn/winter hydrological proxy related to changes of vapor source, precipitation amount, and/or seasonal rainfall distribution, while …
Monitoring in the Barać and Lower Cerovačka caves (Croatia) as a basis for the characterization of the climatological and hydrological processes that control speleothem formation
Monitoring of selected caves as a prerequisite for the speleothem-based reconstruction of the Quaternary environment in Croatia
Holocene hydroclimate changes in continental Croatia recorded in speleothem δ 13 C and δ 18 O from Nova Grgosova Cave
We present the first stable isotope (δ 13 C and δ 18 O) speleothem record from continental Croatia retrieved from two coeval stalagmites from Nova Grgosova Cave. U-Th dates constrain the stalagmite growth history from 10 ka to the present, revealing coeval growth between 7.8 and 5.6 ka. We interpret δ 18 O as an autumn/winter hydrological proxy related to changes of vapor source, precipitation amount, and/or seasonal rainfall distribution, while …
Monitoring in the Barać and Lower Cerovačka caves (Croatia) as a basis for the characterization of the climatological and hydrological processes that control speleothem formation
Monitoring of selected caves as a prerequisite for the speleothem-based reconstruction of the Quaternary environment in Croatia
Holocene hydroclimate changes in continental Croatia recorded in speleothem δ 13 C and δ 18 O from Nova Grgosova Cave
We present the first stable isotope (δ 13 C and δ 18 O) speleothem record from continental Croatia retrieved from two coeval stalagmites from Nova Grgosova Cave. U-Th dates constrain the stalagmite growth history from 10 ka to the present, revealing coeval growth between 7.8 and 5.6 ka. We interpret δ 18 O as an autumn/winter hydrological proxy related to changes of vapor source, precipitation amount, and/or seasonal rainfall distribution, while …
Late Pleistocene - Holocene geomorphologic evolution of the Kvarner area (northern Adriatic, Croatia)
Geology and Paleoclimatology Research (4 works) · Archaeology (3 works) · Cave (3 works) · Geography (3 works) · Geology (3 works) · Precipitation (3 works) · Speleothem (3 works) · Calcite (2 works) · Geochemistry (2 works) · Groundwater and Isotope Geochemistry (2 works)