Arterial faults and their role in mineralizing systems
In quartzo-feldspathic continental crust with moderate-to-high heat flow, seismic activity extends to depths of 10–20 km, bounded by isotherms in the 350–450 °C range. Fluid overpressuring above hydrostatic in seismogenic crust, is heterogeneous but tends to develop in the lower seismogenic zone (ba...
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| Format: | Article |
| Language: | English |
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Elsevier
2019-11-01
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| Series: | Geoscience Frontiers |
| Online Access: | http://www.sciencedirect.com/science/article/pii/S1674987119300386 |