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横贯浙、赣两省的绍兴—江山深断裂被人们认识已有近二十年的历史了。它是浙江广大地质工作者在六十年代初所首先发现的。1964年汪龙文、黄旭林等曾在浙江省地质学会第二届年会上发表专文讨论,沿断裂带各图幅区测报告及浙江石油地质大队的有关材料中也都提到这深断裂并不断补充了新材料。由于证据确凿,目前这一深断裂已为地质界所公认,黄汲清、张文佑、郭令智及乔秀夫等都正确指出本断裂属超岩石圈断裂或岩石圈断裂,属古俯冲带或古缝合线所在。关于深断裂的证据贵阳地化所并根据前人资料
Shaoxing - Jiangshan deep fault crossing Zhejiang and Jiangxi provinces has been recognized for nearly two decades. It was first discovered by geologists in Zhejiang in the early 1960s. In 1964 Wang Longwen, Huang Xulin et al. Published a monograph at the Second Annual Meeting of the Geological Society of Zhejiang Province. Along the fault zones and regional oil and gas geologic survey reports and related materials of the Zhejiang Petroleum Geological Brigade, they also mentioned that this deep fracture is constantly being supplemented New material Due to the evidence, the deep fault has now been recognized by the geological community. Huang Jiqing, Zhang Wenyou, Guo Lingzhi and Qiao Xiufu correctly pointed out that this fault belongs to the super-lithosphere or lithospheric fault and belongs to the ancient subduction zone or ancient suture Where you are. Evidence of deep fracture Guiyang Dushihua and based on previous data