因此，金沙江带不能作为古特提斯域的主缝合带。
It proves that the Jinshajiang suture zone could not have formed the main suture zone in the Paleo-Tethys domain.
它们主要分布在滇西地区的金沙江—哀牢山富碱斑岩带中及附近。
They are mainly distributed along the alkali rich porphyry belt of Jinshajiang Ailaoshan area in western Yunnan.
滇西羊拉铜矿区位于金沙江构造带中部，当时处于活动大陆边缘的半深水斜坡之上。
Located in middle part of the Jinshajiang tectonic belt, the Yangla copper orefield was in the clinoform area of an active continental margin.
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