Geological model of a young volcano-plutonic system: The geothermal region of Monte Amiata (Tuscany, Italy)

Geothermics ◽  
1988 ◽  
Vol 17 (5-6) ◽  
pp. 719-734 ◽  
Author(s):  
Giovanni Gianelli ◽  
Mariano Puxeddu ◽  
Fausto Batini ◽  
Giovanni Bertini ◽  
Ivano Dini ◽  
...  
1962 ◽  
Vol 14 ◽  
pp. 169-257 ◽  
Author(s):  
J. Green

The term geo-sciences has been used here to include the disciplines geology, geophysics and geochemistry. However, in order to apply geophysics and geochemistry effectively one must begin with a geological model. Therefore, the science of geology should be used as the basis for lunar exploration. From an astronomical point of view, a lunar terrain heavily impacted with meteors appears the more reasonable; although from a geological standpoint, volcanism seems the more probable mechanism. A surface liberally marked with volcanic features has been advocated by such geologists as Bülow, Dana, Suess, von Wolff, Shaler, Spurr, and Kuno. In this paper, both the impact and volcanic hypotheses are considered in the application of the geo-sciences to manned lunar exploration. However, more emphasis is placed on the volcanic, or more correctly the defluidization, hypothesis to account for lunar surface features.


2015 ◽  
Vol 35 ◽  
pp. 104-108
Author(s):  
Marta Della Seta ◽  
Carlo Esposito ◽  
Gian Marco Marmoni ◽  
Salvatore Martino ◽  
Antonella Paciello ◽  
...  

Author(s):  
A.B. Popova ◽  
◽  
O.S. Makhova ◽  
N.A. Malyshev ◽  
V.E. Verzhbitskiy ◽  
...  

2019 ◽  
Author(s):  
Andrew Feitz ◽  
Bruce Radke ◽  
Md. Shahadat Hossain ◽  
Brett Harris ◽  
Ralf Schaa ◽  
...  

2016 ◽  
Author(s):  
Schuyler T. Robinson ◽  
◽  
Robert W. Clayton
Keyword(s):  

2021 ◽  
Vol 225 (2) ◽  
pp. 984-997
Author(s):  
Álvaro Osorio Riffo ◽  
Guillaume Mauri ◽  
Adriano Mazzini ◽  
Stephen A Miller

SUMMARY Lusi is a sediment-hosted hydrothermal system located near Sidoarjo in Central Java, Indonesia, and has erupted continuously since May 2006. This mud eruption extends over a surface of ∼7 km2, and is framed by high containment dams. The present study investigates the geometry of the subsurface structures using a detailed gravimetric model to visualize in 3-D the Lusi system and surrounding lithologies. The obtained residual Bouguer anomaly map, simulated through geostatistical interpolation methods, supports the results of previous deformation studies. The negative gravity anomaly zones identified at Lusi are interpreted as fractured areas through which fluids can ascend towards the surface. A 3-D detailed geological model of the area was constructed with Geomodeller™ to highlight the main features. This model relies on the structures’ density contrasts, the interpreted residual Bouguer anomaly map, and geological data from previous authors. 3-D algorithms were used to calculate the gravity response of the model and validate it by inverse methods. The final output is a gravity constrained 3-D geological model of the Lusi mud edifice. These results provide essential details on the Lusi subsurface and may be useful for possible future geothermal resource exploitation and for the risk mitigation plans related to the maintenance of the man-made framing embankment.


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