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1)  thrust sheet-top basin
逆冲席顶盆地
2)  overthrust sheet belt
逆冲席带
1.
This paper has studied the development of setting & model of the overthrust , which is distributed over the plane & section ,and its belting character in the northern margin region of Chaidamu basin , and described the character of the main overthrust sheet belt and lower strain area in great details.
研究了柴北缘地区逆冲推覆构造的发育背景、发育模式 ,平面、剖面展布特征及其分带性 ,并对主干逆冲断裂带及其间的推覆体带、逆冲席带和低应变区的特征进行了详细描述 ,同时通过野外观察和室内构造反演来研究推覆构造的发展演变模式及其形成机理 ,指出其逆冲叠瓦扇带和隐伏逆冲前缘带是最有利的油气勘探目标 图 6,参
3)  broad top basin
宽顶盆地
4)  nappe sheet
逆冲推覆岩席
1.
Cut by a thrust,the Jiaduocuo granodiorite tonalite mass occurs as different forms on three nappe sheets The lithodemic units are established On the basis of lithogenetic age and litology,it is divided into four units which are incorporated into one superunit Make an approach to the compositional polarity from which it is concluded that the Garz Litang junction subducted westward
加多措岩体因逆冲推覆断裂切割、肢解而分布于三个不同的逆冲推覆岩席之上,且产出形态多样。
5)  basinal subduction
盆地俯冲
6)  allochthonous thrust sheet
异地逆掩鳞岩席
补充资料:冲卿席上得行字
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