Hot Flowing Mud Is Terror of Volcano

Numerical modelling of mud volcanoes and

Numerical modelling of mud volcanoes and their flows using constraints from the Gulf of Cadiz

✍ Bramley J. Murton; Juliet Biggs 📂 Article 📅 2003 🏛 Elsevier Science 🌐 English ⚖ 515 KB

It is estimated that the total number of submarine mud volcanoes is between 1000 and 100 000. Because many are associated with greenhouse gases, such as methane, it is argued that the global flux of these gases to the atmosphere from the world's terrestrial and submarine mud volcanoes is highly sign

Corrigendum to “Impact of hot fluid adve

Corrigendum to “Impact of hot fluid advection on hydrocarbon gas production and seepage in mud volcano sediments of thick Cenozoic deltas” [Earth Planet. Sci. Lett. 341–344 (2012) 139–157]

✍ Marianne Nuzzo; Marcus Elvert; Mark Schmidt; Florian Scholz; Anja Reitz; Kai-Uwe 📂 Article 📅 2012 🏛 Elsevier Science 🌐 English ⚖ 72 KB

[IEEE 2008 Second Workshop on Use of Rem

[IEEE 2008 Second Workshop on Use of Remote Sensing Techniques for Monitoring Volcanoes and Seismogenic Areas (USEReST) - Napoli, Italy (2008.11.11-2008.11.14)] 2008 Second Workshop on Use of Remote Sensing Techniques for Monitoring Volcanoes and Seismogenic Areas - Hot spot detection and effusion rate estimation using satellite data to drive lava flow simulations

✍ Vicari, Annamaria; Ganci, Gaetana; Ciraudo, Alessia; Herault, Alexis; Corviello, 📂 Article 📅 2008 🏛 IEEE ⚖ 298 KB

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