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

Michał Krobicki (ed.)
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Abstract

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!!
实地考察-外弗理斯喀尔巴阡山脉和皮宁克里彭带(PKB)
我们很高兴在疫情过后,我们能够在IGCP 710项目第二次专题讨论会期间亲自会面,这打乱了我们定期举行年度会议的想法。在2021年秋季的第一次虚拟会议之后,我们现在有机会面对面讨论,并一起去实地触摸“特提斯”岩石,以便更好地了解数亿年/数十年以前在我们可爱的古老海洋中发生的事情。正如你所知道的,通过你的知识和经验,特提斯海洋的历史,无论是西部还是东部,都是迷人的,但至少可以说,有时是神秘的。一般来说,特提斯洋的地质历史是大致确定的。然而,关于大地构造学、古地理学、古海洋学和古生物地理学的许多细节仍然未知,许多重大问题仍然存在。对大陆和海洋盆地分布的精确重建,以及对特提斯沿岸海路的开合,是对中新生代海洋/气候历史的进一步认识。关于独立盆地的数量和大小,以及它们的时空关系,几乎没有一致意见。此外,对于以前的微大陆的数目和位置以及它们是否并入今天的欧亚山带,也没有达成一致意见。研究这些带各个部分的地质学家是在不同的地质系统中接受教育的,并坚持不同的地质范式。将西特提斯和东特提斯联系起来是很困难的,不仅因为它们相距遥远,而且因为它们被巨大的喜马拉雅碰撞区分开,在这个区域内,许多前古近纪的构造地层信息已经丢失。IGCP项目的目的是将来自前特提斯(摩洛哥/伊比利亚-东南亚)西部和东部的地质学家聚集在一起,建立一个共同的框架和共同的构造地层概念(最新的古生代-中生代,重点是二叠纪-侏罗纪)。一方面,联合国教科文组织为IGCP项目形成了一个特殊的保护伞,另一方面,它多年来一直非常积极地支持“地质公园”和“地质旅游”的理念。出于这个原因,我们决定使用一本国际杂志——地理旅游——来印刷我们的材料,包括摘要和实地旅行指南。我们希望它能对特提斯的朋友和地质旅游爱好者有所帮助。在研讨会的固定部分享受克拉科夫和波兰-斯洛伐克-捷克喀尔巴阡人在5天的实地考察!!
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