Zhang Hong, Ma Junxiao, Quan Heng, Jin Chengzhu. THE DYNAMIC BACKGROUND OF MESOZOIC VOLCANIC ACTIVITY IN NORTHERN PART OF DAXING' ANLING MOUNTAINS[J]. Geology and Resources, 1999, 8(1): 56-64. DOI: 10.13686/j.cnki.dzyzy.1999.01.013
Citation:
Zhang Hong, Ma Junxiao, Quan Heng, Jin Chengzhu. THE DYNAMIC BACKGROUND OF MESOZOIC VOLCANIC ACTIVITY IN NORTHERN PART OF DAXING' ANLING MOUNTAINS[J]. Geology and Resources, 1999, 8(1): 56-64. DOI: 10.13686/j.cnki.dzyzy.1999.01.013
Zhang Hong, Ma Junxiao, Quan Heng, Jin Chengzhu. THE DYNAMIC BACKGROUND OF MESOZOIC VOLCANIC ACTIVITY IN NORTHERN PART OF DAXING' ANLING MOUNTAINS[J]. Geology and Resources, 1999, 8(1): 56-64. DOI: 10.13686/j.cnki.dzyzy.1999.01.013
Citation:
Zhang Hong, Ma Junxiao, Quan Heng, Jin Chengzhu. THE DYNAMIC BACKGROUND OF MESOZOIC VOLCANIC ACTIVITY IN NORTHERN PART OF DAXING' ANLING MOUNTAINS[J]. Geology and Resources, 1999, 8(1): 56-64. DOI: 10.13686/j.cnki.dzyzy.1999.01.013
THE DYNAMIC BACKGROUND OF MESOZOIC VOLCANIC ACTIVITY IN NORTHERN PART OF DAXING' ANLING MOUNTAINS
The Mesozoic volcanic activity in northern Daxing'anling Mts.(NDM) is very violent,in which a lot of geologists are interested The volcanic rocks,formed mainly in Late Jurassic to Early Cretaceous(150~100 Ma),are divided into the Tamulangou formation(J3t),Jixiangfeng formation(J3j),Shangkuli formation(K1s) and Yilikede formation(K1y).