𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Fate of carbonates within oceanic plates subducted to the lower mantle, and a possible mechanism of diamond formation

✍ Scribed by Yusuke Seto; Daisuke Hamane; Takaya Nagai; Kiyoshi Fujino

Book ID
105983152
Publisher
Springer-Verlag
Year
2008
Tongue
English
Weight
332 KB
Volume
35
Category
Article
ISSN
0342-1791

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

The global network of plate boundaries c
The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid-plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains.
✍ L.-E. Ricou 📂 Article 📅 1998 🏛 John Wiley and Sons 🌐 English ⚖ 197 KB

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a sin