The ups and downs of “Tectonic Quiescence”—recognizing differential subsidence in the epicontinental sea of the Oxfordian in the Swiss Jura Mountains
The ups and downs of “Tectonic Quiescence”—recognizing differential subsidence in the epicontinental sea of the Oxfordian in the Swiss Jura Mountains
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“构造静止”的盛衰——认识瑞士汝拉山脉牛津阶陆表海的差异沉降
DOI:
10.1016/s0037-0738(01)00202-0
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发表时间:
2002
影响因子:
2.8
通讯作者:
R. Allenbach
中科院分区:
文献类型:
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作者:
R. Allenbach