New indications of gas hydrate in the northeastern China permafrost zone

• 作者: Chen Liu Dao-gong Hu Fang-yun Song Jian Deng Li Yi Xing-min Zhao Zhi-gang Wen Zhu Rao
• 来源期刊: 中国地质（英文）
• 年，卷（期）: 2018,（2）
• 所属期刊栏目: Research Advances
• 页码范围: 308-309
• 页数: 2页
• 语种: 中文
• DOI: 10.31035/cg2018033

摘要

1. Objectives The Mohe Basin in Heilongjiang, China has a NEE thrust nappe belt, which was assembled by the root zone, middle thrust zone and thrust front, north-south and north-east normal faults with three tectonic activities of the Middle Jurassic to Eocene, the Miocene, and the Early to Middle Pleistocene. The middle thrust zone and thrust front has a large number of folds, thrust faults, fractures and glutenites, which are the major structures of gas hydrate accumulation in the Mohe Basin.