HelioWebUniversity of Parma, Department of Physics and Earth Sciences
flowchart
I[University of Parma, Department of Physics and Earth Sciences]
PI["Parent Institutions (1)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (18)"]
CA["Linked Collaborating Authors (6)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Evidence for KCl Brine Metasomatism in Mafic Xenoliths from the Lower Crust
- Comparison of Numerical and Analogue Models of Thrust Wedges
- Calcareous Nannofossil Evidence for Marine Isotopic Stage 31 (1 Ma) in ANDRILL MIS Core (Western Ross Sea, Antarctica)
- Flood water storage as a resource for agriculture and groundwater recharge: the empting of artificial leaking ponds
- Multidisciplinary seismotectonics of a low-angle normal fault system (Lunigiana- Garfagnana grabens, Italy)
- Spectral and Morphological Analysis of Daedalia Planum Lava Field
- Deep structure and historical earthquakes in the Calabrian subduction zone (Southern Italy): preliminary results from multi-channel seismic reflection profiles
- Late Eocene Antarctic climate variability during the transition to a full glacial state
- MIDDLE EOCENE - EARLY OLIGOCENE PALEOCLIMATE VARIABILITY AT ODP SITE 738 (KERGUELEN PLATEAU) INFERRED BY COMBINED CALCAREOUS NANNOFOSSIL, STABLE ISOTOPE, AND PALEOMAGNETIC DATA
- New evidence of the Monchique - Madeira hot spot volcanism at the Coral Patch seamount, Central Eastern Atlantic Sea
- Isotopic (δ18O, δD and deuterium excess) records from the TALDICE ice core (East Antarctica) (Invited)
- Spectra of volcanic rocks glasses as analogues of Mercury surface spectra
- Dimensional and spatial patterns of disrupted blocks of Messinian gypsum, western Caltanissetta Basin, Sicily
- Magnetotactic bacterial abundance in pelagic marine environments is limited by availability of dissolved iron and organic carbon flux
- Model VNIR optical constants of silicates mixtures analogues to igneous rocks
- Clay minerals in Quaternary marine sediments from the southern Svalbard continental slope: palaeoenvironmental significance
- Constraints on Fault Dynamic Weakening Mechanisms From Natural Slip Surfaces in Carbonate Faults
- Retrieving optical constants of glasses with variable iron abundance