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华北中部太行山带晚中生代时曾有过强烈的火山-深成岩浆活动。本文拟通过对它们原始面貌及演化的分析来探讨当时的构造环境以及它与亚洲东部环太平洋岩浆活动带的关系。
During the Late Mesozoic of the Taihang Mountain belt in central North China, there was intense volcanic-deep magmatic activity. This article intends to explore the tectonic setting at the time and its relationship with the Pacific Rim magmatism belt in eastern Asia by analyzing their original appearance and evolution.