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在鄂霍茨克-楚科奇火山带内带基底中划分出来的科尼-泰戈诺斯古火山带,为晚古生代-晚中生代的岛系,由科尼-泰戈诺斯和穆尔加利两部分组成。本带从西南的乌利伊和鄂霍特两河流的源头,向北东延伸到品仁和阿纳迪尔两河流域,占据了鄂霍茨克海北岸、利相、科尼、皮亚基纳和泰戈诺斯等半岛。在西北部,此构造受南西向的切洛姆贾-雅姆大断裂带控制,在泰戈诺斯半岛上受从北西限定捷兰地堑-向斜的大断裂控制,而在东北部,则受维尔
In the Okhotsk - Chukotka inland belt basement delimitations from the Konyi - Tayunosu ancient volcanic belt, for the Late Paleozoic - late Mesozoic island system, by the Coney - Te Gonnos and Moore Gary composed of two parts. From the source of the two rivers of Uliy and Okhot in the southwest, the belt extends to the north east to the two river valleys of Pinin and Anadir, occupying the northern shore of Okhotsk Sea, Lee phase, Konyi, and Piarjina And Peninsula, such as Tayronos. In the northwestern part, this structure is dominated by the southwesterly El Rocín-Yam fault and controlled by the Great Tenement-Tertiary Great Fault controlled by the North West on the Tegernos Peninsula. In the northeast, By Vail