Pelso Plate or Pelsonia Terrane is a small tectonic unit. It is situated in the Pannonian Basin in Europe. The Carpathian Mountains and the basin surrounded by them were formed from the Cretaceous until the Miocene in the collision of continental Europe with smaller continental fragments of , Tisza, Pelso and . The Zagreb-Hernád line is the former plate margin between the Pelso of African origin and the Tisza Plate of Eurasian origin.
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| - Lempeng Pelso (in)
- Pelso Plate (en)
- 佩索板塊 (zh)
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| - 佩索板块是一个位于欧洲的小型构造单元。喀尔巴阡山脉及环绕它们的山脉约形成于白垩纪至中新世，形成于欧洲大陆与、佩索板块和蒂萨板块的碰撞。萨格勒布-霍尔纳德河线是非洲来源的佩索板块和欧亚来源的蒂萨板块间的古界线。 佩索板块有时会被视作ALCAPA板块的南半部，并与西喀尔巴阡山脉内陆地区相比较。这一区域的典型特征是第纳尔-阿普利亚相三叠纪岩石，而部分文献中，整个Alcapa都属于。 (zh)
- Pelso Plate or Pelsonia Terrane is a small tectonic unit. It is situated in the Pannonian Basin in Europe. The Carpathian Mountains and the basin surrounded by them were formed from the Cretaceous until the Miocene in the collision of continental Europe with smaller continental fragments of , Tisza, Pelso and . The Zagreb-Hernád line is the former plate margin between the Pelso of African origin and the Tisza Plate of Eurasian origin. (en)
- Lempeng Pelso atau Medan Pelsonia adalah bagian tektonik yang kecil. Ini terletak di Cekungan Pannonia. Pegunungan Carpathia dan cekungan mengelilingi tempat ini, terbentuk dari zaman Kapur sampai Miosen dalam tabrakan benua Eropa dengan fragmen benua yang lebih kecil dari , Tisza, Pelso dan . Garis Zagreb- adalah bekas jarak lempeng antara Pelso yang berasal dari Lempeng Afrika, dan Tisza yang berasal dari Lempeng Eurasia. (in)
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| - Pelso Plate or Pelsonia Terrane is a small tectonic unit. It is situated in the Pannonian Basin in Europe. The Carpathian Mountains and the basin surrounded by them were formed from the Cretaceous until the Miocene in the collision of continental Europe with smaller continental fragments of , Tisza, Pelso and . The Zagreb-Hernád line is the former plate margin between the Pelso of African origin and the Tisza Plate of Eurasian origin. The Pelso block is sometimes considered as southern portion of the ALCAPA and compared with internal zone of Western Carpathian Mts. which is called . The typical feature of this zone is Dinaric - Apulian facies of Triassic rocks, while the whole Alcapa is in some papers considered as part of the Apulian plate. The Pelso sensu stricto is therefore composed of , and superunits, that evolved south of the and the superimposed Cenozoic sedimentary cover. (en)
- Lempeng Pelso atau Medan Pelsonia adalah bagian tektonik yang kecil. Ini terletak di Cekungan Pannonia. Pegunungan Carpathia dan cekungan mengelilingi tempat ini, terbentuk dari zaman Kapur sampai Miosen dalam tabrakan benua Eropa dengan fragmen benua yang lebih kecil dari , Tisza, Pelso dan . Garis Zagreb- adalah bekas jarak lempeng antara Pelso yang berasal dari Lempeng Afrika, dan Tisza yang berasal dari Lempeng Eurasia. Lempeng Pelso sering kali dipertimbangkan sebagai bagian selatan dari Alcapa dan dibandingkan dengan zona bagian dalam Pegunungan Carpathia Barat yang disebut . Tipe fisik dari wilayah ini adalah - jenis Apulian dari batuan zaman Triasik, sedangkan di beberapa riset, keseluruhan Alcapa dipertimbangkan sebagai salah satu bagian dari . Pelso terdiri dari bagian besar lempeng tektonik, yaitu , dan , yang berkembang menjadi bagian selatan , dan tumpang-tindih dengan sedimen penutup Kenozoikum. (in)
- 佩索板块是一个位于欧洲的小型构造单元。喀尔巴阡山脉及环绕它们的山脉约形成于白垩纪至中新世，形成于欧洲大陆与、佩索板块和蒂萨板块的碰撞。萨格勒布-霍尔纳德河线是非洲来源的佩索板块和欧亚来源的蒂萨板块间的古界线。 佩索板块有时会被视作ALCAPA板块的南半部，并与西喀尔巴阡山脉内陆地区相比较。这一区域的典型特征是第纳尔-阿普利亚相三叠纪岩石，而部分文献中，整个Alcapa都属于。 (zh)
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