1) aulacogen
拗拉槽
1.
During Sinian Early Paleozoic, three aulacogens within the region formed with the mouths opening toward the northeast.
震旦纪－早古生代发育三个向ＮＥ方向打开的拗拉槽，具有典型的三段式建造序列，槽内沉积作用不同于槽间区域的沉积作用。
2.
The so*$-called “Helan aulacogen” did not occur in the early Paleozoic,and there was not aulacogen there.
分析结果表明 ,该地区在早古生代不是拗拉槽 ,而更可能是北祁连岛弧靠大陆一侧的弧后盆地 ,在晚期演变为弧后前陆盆地。
2) palaeoaulacogen
古拗拉槽
3) North Qilian Aulacogen
北祁连拗拉槽
4) Early Proterozoic aulacogen
早古生代拗拉槽
5) Helan Aulacogen
贺兰拗拉谷
1.
Sequence Stratigraphy and Marine Source Rocks of Cambrian and Ordovician, Helan Aulacogen;
贺兰拗拉谷寒武—奥陶系层序地层及海相烃源岩研究
6) aulacogen structure
拗拉谷构造
补充资料：撒拗
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