冒地槽

卡林型金矿床主要分布在北美大盆地地区科迪勒拉造山带、科罗拉多地台和我国扬子地块西南缘的板内古生代-中生代沉降带和西北缘古生代-中生代冒地槽。

The Carlin-type gold deposits are mostly found in the Cordillera orogen and Colorado platform , Great basin region of North America and Paleozoic-Mesozoic intra-block depressed zone at the southwest margin of the Yangtze block and miogeosyncline northwest of the Yangtze block .

阐述了华南东部震旦－志留纪大地构造属性是大陆边缘弧（优地槽型建造）和弧背盆地（冒地槽型建造）造山带；

It is explained that the Sinian-Silurian geotectonic attribution of the east part of South China is an orogenic belt made up of a continental marginal arc ( eugeosynclinal type formation ) and a retroarc basin ( miogeosynclinal formation ) .

指出洛河地区处于洛南&栾川过渡带的冒地槽沉积盆地，岩相属浅水相碳酸盐台地向大陆斜坡或次深海相过度沉积。

The Luohe area is located in a miogeosynclinal sedimentary basin of the transition region from Luonan to Luanchuan where the facies should be the transitional sediments from the shallow-water facies of the carbonate platform to continental slope or to deep-water facies .