The Qiantang terrane is one of three main west-east-trending terranes of the Tibetan Plateau. During the Triassic, a southward-directed subduction along its northern margin resulted in the , the limit between it and the . During the Late Jurassic and Early Cretaceous, the Lhasa terrane merged with its southern margin along the Bangong suture. This suture, the closure of part of the Tethys Ocean, transformed the Qiantang terrane into a large-scale anticline. The merging of the Lhasa and Qiangtang terranes resulted in the uplift of a palaeoplateau known as the Qiangtang Plateau, which rapidly thinned later in the Cretaceous.
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| - Plaque de Qiantang (fr)
- Placca di Qiantang (it)
- Qiangtang terrane (en)
- 羌塘地块 (zh)
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| - La placca di Qiantang era un'antica placca tettonica della litosfera terrestre. (it)
- 羌塘地块是青藏高原3个主要东西向地体之一。 反映三叠纪时羌塘地块北缘向南，潜没到下方。在侏罗纪，拉萨地体与羌塘地块的南缘沿熔合。这一缝合带也是特提斯洋的闭合线，使羌塘地块变成了巨大的背斜。 羌塘地块目前海拔约5km，不过其抬升的具体时间存在争议，从上新世-更新世(3–5 Ma)到始新世(35 Ma)的估计都有。后者的估计基于高原第一次遭受剥蚀作用的时间。 (zh)
- La plaque de Qiantang est une ancienne plaque tectonique de la lithosphère de la planète Terre. Elle a existé durant le Mésozoïque et est entrée en collision avec la plaque eurasienne située au Nord au début du Jurassique alors que les plaques indienne et de Lhassa situées au Sud remontaient vers le Nord. On ne sait pas comment a réagi la plaque de Qiantang avec la plaque cimmérienne qui s'est également soudée au Sud de la plaque eurasienne. Au Sud, la plaque de Lhassa disparaissait par subduction sous la plaque de Qiantang et au Nord, la plaque de Qiantang disparaissait par subduction sous la plaque eurasienne. (fr)
- The Qiantang terrane is one of three main west-east-trending terranes of the Tibetan Plateau. During the Triassic, a southward-directed subduction along its northern margin resulted in the , the limit between it and the . During the Late Jurassic and Early Cretaceous, the Lhasa terrane merged with its southern margin along the Bangong suture. This suture, the closure of part of the Tethys Ocean, transformed the Qiantang terrane into a large-scale anticline. The merging of the Lhasa and Qiangtang terranes resulted in the uplift of a palaeoplateau known as the Qiangtang Plateau, which rapidly thinned later in the Cretaceous. (en)
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| - La plaque de Qiantang est une ancienne plaque tectonique de la lithosphère de la planète Terre. Elle a existé durant le Mésozoïque et est entrée en collision avec la plaque eurasienne située au Nord au début du Jurassique alors que les plaques indienne et de Lhassa situées au Sud remontaient vers le Nord. On ne sait pas comment a réagi la plaque de Qiantang avec la plaque cimmérienne qui s'est également soudée au Sud de la plaque eurasienne. Au Sud, la plaque de Lhassa disparaissait par subduction sous la plaque de Qiantang et au Nord, la plaque de Qiantang disparaissait par subduction sous la plaque eurasienne. La plaque de Qiantang forme aujourd'hui le Nord du plateau tibétain. (fr)
- The Qiantang terrane is one of three main west-east-trending terranes of the Tibetan Plateau. During the Triassic, a southward-directed subduction along its northern margin resulted in the , the limit between it and the . During the Late Jurassic and Early Cretaceous, the Lhasa terrane merged with its southern margin along the Bangong suture. This suture, the closure of part of the Tethys Ocean, transformed the Qiantang terrane into a large-scale anticline. The merging of the Lhasa and Qiangtang terranes resulted in the uplift of a palaeoplateau known as the Qiangtang Plateau, which rapidly thinned later in the Cretaceous. The Qiantang terrane is now located at c. 5,000 m (16,000 ft) above sea level, but the timing of this uplift remains debated, with estimates ranging from the Pliocene-Pleistocene (3–5 Mya) to the Eocene (35 Mya) when the plateau was first denudated. (en)
- La placca di Qiantang era un'antica placca tettonica della litosfera terrestre. (it)
- 羌塘地块是青藏高原3个主要东西向地体之一。 反映三叠纪时羌塘地块北缘向南，潜没到下方。在侏罗纪，拉萨地体与羌塘地块的南缘沿熔合。这一缝合带也是特提斯洋的闭合线，使羌塘地块变成了巨大的背斜。 羌塘地块目前海拔约5km，不过其抬升的具体时间存在争议，从上新世-更新世(3–5 Ma)到始新世(35 Ma)的估计都有。后者的估计基于高原第一次遭受剥蚀作用的时间。 (zh)
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