Mesozoic paleomagnetic data from the Transdanubian Range Unit (TRU) of the Pannonian Basin has been revised and updated to enable its paleogeographic evolution within SE Europe to be evaluated. After a 30° declination correction, the TRU data are fully consistent with those for Adria which has an almost identical stratigraphic history. This enabled a revised Apparent Polar Wander Path (APWP) to be constructed for the combined data. Comparing this with the corresponding African and European APWP shows that Adria separated from Europe around 190 Ma, then moved independently southwards between 170–120 Ma (a 30° clockwise rotation changing to counter-clockwise around 155–145 Ma). After 155 Ma, there was a northward movement that brought Adria close to the stable European margin by 115 Ma. This latter may have been with or independently of Africa. After 100 Ma, Africa and Adria moved in coordination until the end of the Cretaceous. This sequence of events correlated well with geologically established tectonic events. These include the major extensional phases in the Alpine Tethys during the southward shift and large clockwise rotation (170–155/145 Ma). This was followed by ophiolite obduction in the Neotethys (West and East Vardar) around 155–145 Ma as a result of the dramatic reversal in the displacement of Adria. Finally, around 115 Ma, the TRU was emplaced over Austroalpine units as a thick nappe associated with the general uplift in the Adriatic realm.

中文翻译：

---

亚德里亚的新中生代 APWP 由来自外多瑙河山脉单元的数据辅助 - 欧洲-非洲地球动力学系统的构造解释


来自潘诺尼亚盆地跨多瑙河山脉单元 （TRU） 的中生代古地磁数据已经过修订和更新，以便能够评估其在欧洲东南部的古地理演变。经过 30° 赤纬校正后，TRU 数据与 Adria 的数据完全一致，后者的地层历史几乎相同。这使得能够为组合数据构建修订后的视极地漂移路径 （APWP）。将其与相应的非洲和欧洲 APWP 进行比较，显示亚德里亚在 190 马 左右与欧洲分离，然后在 170-120 马 之间独立向南移动（顺时针旋转 30° 变为逆时针旋转，约为 155-145 马）。155 马之后，向北移动，使亚德里亚以 115 马接近稳定的欧洲边缘。后者可能与非洲有关或独立于非洲。100 马后，非洲和亚德里亚协调移动，直到白垩纪末期。这一系列事件与地质学上确定的构造事件密切相关。其中包括阿尔卑斯山特提斯在南移和大顺时针旋转（170-155/145 马）期间的主要伸展阶段。随后，由于亚德里亚岛位移的戏剧性逆转，155-145 马左右在 Neotethys（西和东瓦尔达）发生了蛇绿岩俯冲。最后，在115 马左右，TRU被放置在南方阿尔卑斯山单元上，作为与亚得里亚海地区普遍隆起相关的厚垫。