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OALib Journal期刊
ISSN: 2333-9721
费用：99美元
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昆特依凹陷中生界、新生界发育特征及构造演化分析
Keywords: 柴达木盆地,昆特依凹陷,潜伏构造,构造演化
Abstract:
？昆特依凹陷位于柴达木盆地北缘断块带西段，紧邻冷湖和鄂博梁—葫芦山构造带，是柴达木盆地西北部重要的油气勘探潜力区域。通过对昆特依凹陷内部中生代、新生代地层分布特征的分析，结合地震资料地质解释，认为在中生代末造山后的陆内调整时期，昆特依凹陷内分割性断块发育，形成压陷型分隔性断块坳陷；新生代喜马拉雅构造运动对柴达木盆地的影响主要表现为压扭性构造应力场的作用，伴随阿尔金走滑断裂的活动，昆特依凹陷受其影响和制约，发育形成压陷型沉降坳陷。昆特依凹陷内的潜伏背斜构造在新生代早期开始发育，第四纪最终定型。
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