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Pomeranian basin (NW Poland) and its sedimentary evolution during Mississippian times by Hanna Matyja is a Earth and Planetary Sciences article available to read on EtoBox.
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## Abstract The Carboniferous sedimentary history of the Pomeranian Basin (NW Poland) begins with Hastarian open‐marine carbonates and is terminated with ?lower Asbian terrestrial deposits in the north‐eastern part and, ?upper Asbian or Brigantian, open‐marine shales in the south‐western part of the basin. The ?latest Viséan, Serpukhovian and early Bashkirian was a period of regional non‐deposition and erosion. In the Upper Bashkirian–Gzhelian strata, an alluvial depositional environment was recognized. The Mississippian depositional history of the area has been punctuated by several, regional‐scale events: (1) during the late Famennian–early Tournaisian times anoxic conditions developed over the entire basin. The results of both conodont and miospore studies show the presence of a stratigraphic gap within this sequence (which also show extremely reduced thicknesses), that comprises the uppermost Famennian (Middle and Upper __praesulcata__ conodont zones) and the lowermost Hastarian (__sulcata–sandbergi__ conodont zones). This stratigraphic gap probably resulted from some chemical and/or hydrodynamical factors rather than from any tectonic uplift; (2) volcanic activity on the nearb
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It is typically read by researchers, students, and practitioners in Earth and Planetary Sciences.
- Author
- Hanna Matyja
- Publisher
- John Wiley and Sons; Wiley (John Wiley & Sons); John Wiley & Sons Inc.; Wiley (ISSN 0072-1050)
- Published
- 2008
- Language
- EN
- Field
- Earth and Planetary Sciences (Physical Sciences)