Paleoproterozoic crustal evolution of the Hengshan–Wutai–Fuping region, North China Craton
An arguable point regarding the Neoarchean and Paleoproterozoic crustal evolution of the North China Craton (NCC) is whether the tectonic setting in the central belt during the mid-Paleoproterozoic (2.35–2.0 Ga) was dominated by an extensional regime or an oceanic subduction–arc regime. A review of...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Elsevier
2014-07-01
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| Series: | Geoscience Frontiers |
| Subjects: | |
| Online Access: | http://www.sciencedirect.com/science/article/pii/S1674987114000358 |