Gogolin Formation

Historical name coming from Gogolin, a small town in south Poland, where the Gogolin Formation was described for the first time, and where the main stratotypes have been exposed (see section Stratotypes).

{{Infobox settlement

| name = Gogolin

| settlement_type = Town

| total_type =  

| subdivision_type = Country

| subdivision_name = Poland

| subdivision_type1 = Voivodeship

| subdivision_name1 = Opole

| subdivision_type2 = County

| subdivision_name2 = Krapkowice

| subdivision_type3 = Gmina

| subdivision_name3 = Gogolin

| pushpin_map = Poland

| coordinates = {{coord|50|29|N|18|02|E|region:PL|display=inline}}

}}

The Late Olenekian or Early Aegean (Anisian) to Pelsonian (Anisian),.{{cite journal | last1 = Nawrocki | first1 = J. | last2 = Szulc | first2 = J. | year = 2000 | title = The Middle Triassic magnetostratigraphy from the Peri-Tethys basin in Poland | journal = Earth and Planetary Science Letters | volume = 182 | pages = 77–92 | doi=10.1016/s0012-821x(00)00230-2}}{{cite journal | last1 = Zawidzka | first1 = K | year = 1975 | title = Conodont stratigraphy and sedimentary environment of the Muschelkalk in Upper Silesia | journal = Acta Geologica Polonica | volume = 25 | pages = 217–256 }}

The formation is built of various carbonates which were deposited on a carbonate ramp.Kowal-Linka, M., Stawikowski, W., 2013. Garnet and tourmaline as provenance indicators of terrigenous material in

epicontinental carbonates (Middle Triassic, S Poland), 291: 27–47

File:Gogolin Formation 1.png

This Formation has recently been divided into four members, six beds, and two horizons:

1. Zakrzów Crinoidal Limestone Member, which includes: a) Krapkowice Pelitic Limestone Bed – thin-bedded, wavy bedded and marly micritic limestones, b) Dąbrówka Bioclastic Limestone Bed – thick- to medium-bedded, cross-bedded crinoidal limestones, c) Podbór Bioclastic Limestone Bed – thin- to medium-bedded, graded, horizontally and cross-bedded bioclastic limestones and wavy-bedded micritic limestones;
2. The Skała Marl Member – marls interbedded with micritic and bioclastic limestones; the lowermost part of this member is locally built of broken-up limestone beds and lumps which are covered by an intraformational conglomerate with small intraclasts – they are divided as Kocina Intraformational Conglomerate Bed;
3. The Emilówka Cellular Limestone Member, which includes: a) Karłubiec Bioclastic Limestone Bed – massive, cross-bedded, thin- to medium-bedded bioclastic and micritic limestones, b) Otmęt Marly Limestone Bed – strongly porous, thin-bedded marly limestones that are, in fact, dedolomitized dolomites;
4. Odrowąż marly limestone horizon – marls, thin- to medium-bedded, graded, cross-bedded and horizontally bedded bioclastic limestones and thin layers of platy and wavy bedded micritic limestones;
5. Malnia limestone horizon – thin- to medium-bedded, graded, horizontally and cross-bedded bioclastic limestones, thin-bedded, platy and wavy-bedded micritic limestones;
6. Ligota Hill Wavy-Bedded Limestone Member – wavy-bedded and crumpled micritic limestones intercalated with medium- to thin-bedded, graded, cross- and horizontally bedded, bioclastic limestones.

Stratotypes are located at Gogolin and its vicinity, Błotnica Strzelecka and Ligota Dolna (southern Poland).

{{Reflist}}

• Assmann P., 1913 – Beitrag zur Kenntniss der Stratigraphie des oberschlesischen Muschelkalks. Jb. Preuss. Geol. Landesanst., 34: 658 – 671, Berlin.
• Assmann P., 1944. Die Stratigraphie der oberschlesischen Trias. Teil 2: Der Muschelkalk. Abhandlungen des Reichsamtes für Bodenforschung, Neue Folge, 208: 1–124.
• Kowal-Linka M. 2008. Formalizacja litostratygrafii formacji gogolińskiej (trias środkowy) na Śląsku Opolskim. Geologos 14 (2): 125–161 (and the references; the paper in Polish with English summary).
• Kowal-Linka M. 2009. Nowe jednostki litostratygraficzne w randze warstw w obrębie formacji gogolińskiej (trias środkowy) na Śląsku Opolskim. Geologia 35 (2): 153-174 (and the references; the paper in Polish with English summary).
• Kowal-Linka, M., Stawikowski, W., 2013. Garnet and tourmaline as provenance indicators of terrigenous material in epicontinental carbonates (Middle Triassic, S Poland), 291: 27–47.
• {{cite journal | last1 = Nawrocki | first1 = J. | last2 = Szulc | first2 = J. | year = 2000 | title = The Middle Triassic magnetostratigraphy from the Peri-Tethys basin in Poland | journal = Earth and Planetary Science Letters | volume = 182 | pages = 77–92 | doi=10.1016/s0012-821x(00)00230-2}}
• Niedźwiedzki R., 2000: Litostratygrafia formacji górażdżańskiej i formacji dziewkowickiej na Śląsku Opolskim. Prace Geologiczno-Mineralogiczne, 71, 1–72 (and the references; the paper in Polish with English summary).
• {{cite journal | last1 = Zawidzka | first1 = K | year = 1975 | title = Conodont stratigraphy and sedimentary environment of the Muschelkalk in Upper Silesia | journal = Acta Geologica Polonica | volume = 25 | pages = 217–256 }}

• http://www.geologos.com.pl/archive.php?issue=11
• http://journals.bg.agh.edu.pl/GEOLOGIA/index.php?vol=2009-02
• {{cite journal | doi=10.1016/j.sedgeo.2013.03.005 | volume=291 | title=Garnet and tourmaline as provenance indicators of terrigenous material in epicontinental carbonates (Middle Triassic, S Poland) | journal=Sedimentary Geology | pages=27–47| year=2013 | last1=Kowal-Linka | first1=Monika | last2=Stawikowski | first2=Wojciech }}

Category:Triassic Poland

Category:Triassic System of Europe

Category:Anisian Stage