结合柴北缘区域地质特点，建立了封盖层评价标准。
The evaluation criterion of the cap rock was established, combining the geology feature of the Northern Qaidam Basin;
矿床形成与柴北缘区域地壳多阶段演化和多次成矿作用有关，属多因复成矿床。
The deposit belongs to a poly genetic compound gold deposite resulting from multi mineralizations and its formation is associated with multi stages evolution of the crust in the area.
结果表明：晚侏罗世之后，柴北缘主要受东西方向的挤压，这与区域上的研究结果一致；
The results suggest that the northern Qaidam basin mainly experienced E-W compression after the Middle-Late Jurassic, which is in accordance with previous results.
柴北缘现今构造格局可以划分为三大构造带和两大沉降带，流体势的变化也有相同的特点。
Tectonic configuration in the northern area of Qaidam can be divided into three structural belts and two depressions, which controlled the fluid potential.
这一问题不仅影响着对于整个柴北缘的地质历史的认识，也直接制约着我们对该区的评价和勘探部署。
This issue influenced the geological history of the whole North Qaidam, also directly restricts us on the evaluation and exploration.
昆2井是柴达木盆地北缘昆特依i号构造上的一口风险深探井，井深为5950米，是目前柴北缘最深一口探井。
Kun 2 well with the depth of 5950 meters is the deepest risky exploration well located at the Kunteyi structure I on the northern Qaidam Basin.
昆2井是柴达木盆地北缘昆特依i号构造上的一口风险深探井，井深为5950米，是目前柴北缘最深一口探井。
Kun 2 well with the depth of 5950 meters is the deepest risky exploration well located at the Kunteyi structure I on the northern Qaidam Basin.
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