Jacek Matyszkiewicz
Biographic Data
| ID | 6920237 |
|---|---|
| NAME | Jacek Matyszkiewicz |
| GIVEN NAMES | Jacek |
| FAMILY NAME | Matyszkiewicz |
| SIGNATURE | MATYSZKIEWICZ J |
| AFFILIATIONS | AGH University of Krakow |
| ORCID | 0000-0002-1812-9967 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 2 |
| AUTHOR COUNT | 2 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2020 |
| LATEST PUBLICATION YEAR | 2020 |
| H-INDEX | 1 |
Siliceous rocks from the southern part of the Kraków-Częstochowa Upland (Southern Poland) as potential raw materials in the manufacture of stone tools – A characterization and possibilities of identif…
The Upper Jurassic sediments from the Kraków-Częstochowa Upland developed as carbonates, mostly limestones, which represent the microbial-sponge megafacies that were typical of the northern margin of the Tethys Ocean. Outcrops of these rocks are scattered along an extended belt ranging from Portugal to the Caucasus Mts. One of the common features of the bedded limestones belonging to this megafacies is the local occurrence of chert concretions. T…
The provenance of siliceous rocks from the Kraków-Częstochowa Upland (Poland) used as raw-materials in the manufacture of siliceous artefacts from Central-Eastern Europe; An old problem in new light
One of the siliceous raw-materials used in the manufacture of artefacts and found in archaeological sites in Central-Eastern Europe is the “Jurassic flint from around Kraków” type, the origin of which is believed to be outcrops of Upper Jurassic sediments scattered throughout the southern part of the Kraków-Częstochowa Upland (Southern Poland). Unfortunately, the identification criteria of this siliceous rock remain unclear, which precludes it be…
Siliceous rocks from the southern part of the Kraków-Częstochowa Upland (Southern Poland) as potential raw materials in the manufacture of stone tools – A characterization and possibilities of identif…
The Upper Jurassic sediments from the Kraków-Częstochowa Upland developed as carbonates, mostly limestones, which represent the microbial-sponge megafacies that were typical of the northern margin of the Tethys Ocean. Outcrops of these rocks are scattered along an extended belt ranging from Portugal to the Caucasus Mts. One of the common features of the bedded limestones belonging to this megafacies is the local occurrence of chert concretions. T…
The provenance of siliceous rocks from the Kraków-Częstochowa Upland (Poland) used as raw-materials in the manufacture of siliceous artefacts from Central-Eastern Europe; An old problem in new light
One of the siliceous raw-materials used in the manufacture of artefacts and found in archaeological sites in Central-Eastern Europe is the “Jurassic flint from around Kraków” type, the origin of which is believed to be outcrops of Upper Jurassic sediments scattered throughout the southern part of the Kraków-Częstochowa Upland (Southern Poland). Unfortunately, the identification criteria of this siliceous rock remain unclear, which precludes it be…
Siliceous rocks from the southern part of the Kraków-Częstochowa Upland (Southern Poland) as potential raw materials in the manufacture of stone tools – A characterization and possibilities of identif…
The Upper Jurassic sediments from the Kraków-Częstochowa Upland developed as carbonates, mostly limestones, which represent the microbial-sponge megafacies that were typical of the northern margin of the Tethys Ocean. Outcrops of these rocks are scattered along an extended belt ranging from Portugal to the Caucasus Mts. One of the common features of the bedded limestones belonging to this megafacies is the local occurrence of chert concretions. T…
The provenance of siliceous rocks from the Kraków-Częstochowa Upland (Poland) used as raw-materials in the manufacture of siliceous artefacts from Central-Eastern Europe; An old problem in new light
One of the siliceous raw-materials used in the manufacture of artefacts and found in archaeological sites in Central-Eastern Europe is the “Jurassic flint from around Kraków” type, the origin of which is believed to be outcrops of Upper Jurassic sediments scattered throughout the southern part of the Kraków-Częstochowa Upland (Southern Poland). Unfortunately, the identification criteria of this siliceous rock remain unclear, which precludes it be…
Archaeology (2 works) · Geochemistry (2 works) · Geography (2 works) · Geology (2 works) · Mineralogy and Gemology Studies (2 works) · Outcrop (2 works) · Paleontology (2 works) · Paleontology and Stratigraphy of Fossils (2 works) · Diagenesis (1 works) · Facies (1 works)