The geotourist attractions in the vicinity of Szczawnica spa

Golonka, Jan; Waśkowska, Anna; Doktor, Marek; Krobicki, Michał; Słomka, Tadeusz

doi:10.7494/geotour.2014.37.33

Cited by 2 publications

(2 citation statements)

References 6 publications

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“…The Lower Paleozoic greenschists of deep-sea origin were unconformably covered in many localities by Devonian redbeds. The first time the ICB collided with the SCB during the collisional process is likely to have been in the Late Silurian-Early Devonian times (Golonka et al, 2023). The Song Chay complex granitoid is connected to this event.…”

Section: The Collision Between the Scb And Icb Based On Global Plate ...mentioning

confidence: 98%

Zderzenie bloków Indochin i południowych Chin w północno-zachodnim Wietnamie i związane z nim kontrowersje

HUNG,

GOLONKA,

Nguyen

2023

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Orogeneza indochińska, uznawana za zdarzenie kolizyjne pomiędzy płytami południowych Chin i Indochin, które miało miejsce w rejonie Azja Południowo-Wschodnia, w tym w Wietnamie, doprowadziła do powstania indochińskiego pasma górskiego. Jednak pytanie ilu ile razy w przeszłości doszło do zderzenia tych płyt i w którym okresie pozostaje bez odpowiedzi. Co więcej, zamknięcie starożytnego oceanu i ślady jego pozostałości pomiędzy płytami południowych Chin i Indochin są nadal przedmiotem poważnej debaty. Pochodzenie indochińskiego termotektonizmu jest niepewne. Cały region został dotknięty procesami termotektonicznymi na zachodzie, powstały w wyniku zderzenia płyty Sibumasu z blokiem Indochin. Badanie orogenzezy przeprowadzono z wykorzystaniem paleogeografii, a także paleontologii oraz danych termochronicznych. Nie ma jednoznacznych dowodów sugerujących, że bloki Indochin i Chin Południowych zderzyły się w okresie triasu. Preferowany jest scenariusz płyt tektonicznych, który opisuje orogenezę indochińską jako zdarzenie reaktywacyjne wywołane akrecją bloku Sibumasu do Indochin.

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Section: The Collision Between the Scb And Icb Based On Global Plate ...mentioning

confidence: 98%

Zderzenie bloków Indochin i południowych Chin w północno-zachodnim Wietnamie i związane z nim kontrowersje

HUNG,

GOLONKA,

Nguyen

2023

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“…Very little ichnological data come from radiolarites, however lately Kakuwa (2004) presented their ichnofabric from the Triassic and Jurassic of Japan. One of the major attraction of the PKB region is the rafting through the Dunajec River Gorge (Golonka & Krobicki, 2007; see also Alexandrowicz & Alexandrowicz, 2004). The rafting trip on the Dunajec River, which starts at Sromowce Kąty harbour, takes geotourist through the Dunajec Gorge to Szczawnica.…”

Section: Stop 5 -Biała Woda Valley (Waterfall) -mentioning

confidence: 99%

Field trip – Outer Flysch Carpathians and Pieniny Klippen Belt (PKB)

Krobicki (ed.)

2023

geotour

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We are glad that we can meet personally during the 2nd Symposium of the IGCP 710 Project, after the pandemic time, which disrupted our idea of regular, annual meetings. After the 1st virtual meeting during the autumn of 2021, we have now the chance to discuss face to face and go to the field together to touch „Tethyan” rocks for a better understanding of what happened hundreds/decades of millions years ago in our lovely ancient ocean. As you know, through your knowledge and experience, the Tethyan Ocean history, both in its western and eastern parts, is fascinating, but enigmatic from time to time, to say the least.Generally, the geological history of the Tethys Ocean is broadly established. Yet many details are still unknown and many major questions remain, related to geotectonics, palaeogeography, palaeoceanography and palaeobiogeography. Improved understanding of the Mesozoic-Cenozoic ocean/climate history is based on accurate reconstruction of the distribution of continents and ocean basins and on opening and closing of seaways along the Tethys. There is little or no agreement about the number or size of separate basins, nor on their space-time relationships. Moreover, there is no consensus on the number and location of former micro-continents and on their incorporation into the present-day Eurasian-Mountain Belt. Geologists studying individual parts of these belts have been educated within different geological systems and adhere to different geological paradigms. Correlation between Western and Eastern Tethys is difficult, not only because of the large distances involved, but also because they are separated by the area of the huge Himalayan collision within which much of the pre-Paleogene tectonostratigraphic information has been lost. The aim of this IGCP project is to bring together geologists from the western and eastern parts of the former Tethys (Morocco/Iberia–SE Asia) to establish a common framework and a common tectonostratigraphic concept (latest Paleozoic–Mesozoic with emphasis on Permian–Jurassic).On the one hand, UNESCO forms a special umbrella for the IGCP Projects, and on the other hand, it has been very active in supporting the ideas of “geoparks” and “geotourism” for years. For this reason, we decided to use an international magazine – Geotourism – to print our materials, both abstracts and a field trip guidebook. We hope it will be useful for both Tethyan friends and geotourism enthusiasts.Enjoy Krakow during the stationary part of the Symposium and the Polish-Slovak-Czech Carpathians during a 5-day field trip!!

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The geotourist attractions in the vicinity of Szczawnica spa

Abstract: The main aim of this paper is presentation of the most

Cited by 2 publications

References 6 publications

Zderzenie bloków Indochin i południowych Chin w północno-zachodnim Wietnamie i związane z nim kontrowersje

Zderzenie bloków Indochin i południowych Chin w północno-zachodnim Wietnamie i związane z nim kontrowersje

Field trip – Outer Flysch Carpathians and Pieniny Klippen Belt (PKB)

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