重力、航磁、地震、遥感、地表地质等资料的研究结果表明，柴达木盆地基底存在着中央断裂带。
Based on data of gravity survey, seismic exploration, aerial magnetical survey and surface geology, the central fault belt was identified in the Qaidam Basin.
而中央凹陷带和西部断裂带发育与过剩压力有关的中组合油气分布模式。
The middle combination pattern is developed in the central depression belt and western fracture belt.
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