HelioWebPolish Geological Institute
flowchart
I[Polish Geological Institute]
PI["Parent Institutions (0)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (16)"]
CA["Linked Collaborating Authors (3)"]
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
- <SUP>10</SUP>Be Dating of the Last Retreat of the Southern Margin of the Scandinavian Ice Sheet: Preliminary Results
- Preliminary <SUP>10</SUP>Be Chronology for the Last Deglaciation of the Southern Scandinavian Ice Sheet
- Late Neoproterozoic Paleogeography of the Western Part of Baltica- Constraints From Paleomagnetic and Tectonic Analysis.
- Fluid speciation controls of low-temperature copper isotope fractionation
- Magnetic Susceptibility and Geochemistry of Soils and Alluvial Sediments in the Area of Vistula River Delta (N Poland).
- Contemporary Rigidity of Precambrian and Paleosoic Platform on the Area of Poland on the Base of GPS Data
- Paleomagnetism and Thermal History of the Permian Succession of the Velebit Mts (Dinarides, Croatia)
- Entrainment and Survival Time of the Llsvps: Effects of Flow in the Thermochemical Pile Interior
- Constraints in calculations of evaporative losses in arid climates using the stable isotope composition of water
- The uncertainty of the reflection seismic imaging from analysis of wide-angle post-critical reflections
- Operational exploitation of the Sentinel-1 mission: implications for geoscience
- Integrated PSV, <SUP>14</SUP>C, Pollen Study of the IODP Expedition 347, site M0059 at Little Belt, Baltic Sea, for the last 9000 years.
- Paleomagnetic and magnetic fabric studies of Lower Triassic red sandstones from the autochthonous cover of the Central Western Carpathians: new insights into paleogeographic setting and tectonic evolution of the area
- Is the Mosselhalvøya thrust a major boundary between West Ny-Friesland and Nordaustlandet terranes of the Svalbard Caledonides?
- Why does magnetostratigraphy not work in the Devonian?
- The Devonian magnetic field: weak and poorly understood