HelioWebTechnical University of Marche, Ancona, Italy
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I[Technical University of Marche, Ancona, Italy]
PI["Parent Institutions (0)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (28)"]
CA["Linked Collaborating Authors (5)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
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Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Geochemical Comparison of Late Pliocene Sapropels from Vrica (Calabria) and ODP Site 964.
- Is Productivity Important to Sapropel Deposition? Evidence from Ionian Basin i-cycle 180.
- Late Pleistocene/Holocene Planktonic Assemblages in three Box-Cores from the Mediterranean Ridge Area (S-SW of Crete): Paleoecological and Paleoceanographic Reconstruction of Sapropel S1 Interval
- Paleoclimatic and Paleoceanographic Significance of the Cretaceous Black Shales: a Parallelism with the Neogene Mediterranean Sapropel
- Stable-Isotope Analysis of Italian Shallow-Water Carbonates: the Response of Mesozoic Platform Carbonates to Oceanic Anoxic Events
- Handling Subsurface Transport in Nonstationary Velocity Fields
- Two dimensional hydrological simulation in elastic swelling/shrinking peat soils
- Robustness of Solutions of Head and Velocity Fields Obtained by SFEM in Bounded Random Porous Media
- Simulations of non ergodic transport induced by inhomogeneous flow fields in heterogeneous porous formations of hierarchical sedimentary architecture
- Impact of Uncertainty on the Porous Media Description in the Subsurface Transport Analysis
- 3-D heterogeneous field data versus 2-D simulations. How can it be accomplished in a sedimentary porous formation?
- Is it possible to use different data types and scales to reduce flow and transport uncertainty in natural heterogeneous formations? The experimental setup of the Settolo aquifer (Italy)
- Magnetostratigraphy of the Plio-Pleistocene global stratotype section at Vrica (Italy): magnetic iron sulphides and complex magnetic polarity patterns
- From the local to the regional scale. What is the effect of missing vertical heterogeneity moving from fully 3-D to 2-D depth averaged dispersion models?
- Field Analogues of Shallow-water Hydrocarbon Seepages in the Pleistocene Argille Azzurre Formation: the Chimneys Field of Enza River, Northern Apennines, Italy
- A High-Resolution Upper Pleistocene Palaeomagnetic Record from the Fronte Section at Taranto, Italy
- Connecting marine productivity to sea-spray via microscale biological processes: phytoplancton demise and viral infection
- Common Era Hydroclimate and Atmospheric Circulation in the Western Mediterranean Basin
- Hysteretic behavior in seawater intrusion in response to discontinuous drought periods
- Impact of Fe(III)-OM complexes and Fe(III) polymerization on SOM pools reactivity under different land uses
- Intercomparison of Chemical Multiphase Box Models
- Soil Organic Matter-Mineral interactions across pools in different land uses: the importance of Fe mineral dynamics in natural environments
- Benthic Microbial Community Structure across the Adriatic Sea: Role of Terrigenous Inputs and Human Impacts
- Observation of Potential Transversal Seiching Activity in the Adriatic Sea and Connection to Bora Winds
- Observations of Turbidity Maximum Zones in a Microtidal Environment
- Theoretical and Numerical Investigations into the role of Bora Winds in generating Transversal Seiches in the Adriatic Sea
- Characterizing the Basal Melting Spatio-Temporal Variability of the Ross Ice Shelf using a Regional Ocean Model
- On the Generation of Adriatic Seiches by Bora Winds