Granitic Pegmatites, August 2012, Vol. 8, No. 4
June 28, 2024
Kaolin, June 2014, Vol. 10, No. 3
June 28, 2024
Serpentinites, April 2013, Vol. 9, No. 2
$20.00
Serpentinites, primarily composed of serpentine minerals and formed by hydration of peridotites, increasingly attract the attention of a wide range of scientists, including geophysicists, structural geologists, engineers, and astrobiologists. As serpentinites have wide stability fields, they form in a variety of environments, from the Earth’s surface to the interior of the mantle.
Serpentinites
April 2013, Vol. 9, No. 2
Serpentinites, primarily composed of serpentine minerals and formed by hydration of peridotites, increasingly attract the attention of a wide range of scientists, including geophysicists, structural geologists, engineers, and astrobiologists. As serpentinites have wide stability fields, they form in a variety of environments, from the Earth’s surface to the interior of the mantle. They are important as reservoirs of water in the deep mantle and in the recycling of elements in subduction zones. Because of their physical properties, serpentinites play important roles in seismic activity and geodynamics, including earthquakes in subduction zones, rifting, oceanic spreading, strike-slip faulting, and the exhumation of deeply subducted rocks. Serpentinites are also economically important because obducted serpentinites contain more than half the world’s reserves of nickel.
Why You’ll Love Elements Magazine:
- Expert Contributors: Articles written by renowned researchers in the field of geoscience.
- Engaging Content: Join a community of readers who are passionate about Elements.
- Exceptional Quality: Each issue is printed on high-quality paper with stunning visuals and detailed illustrations that bring complex scientific concepts to life.
Order your copy of the April 2013 issue of Elements magazine today and discover the world of serpentinites.
Related products
-
Platinum-Group Elements, August 2008, Vol. 4, No. 4
$20.00The geoscientific and economic significance of the PGE is immense. Due to their extreme siderophile and chalcophile behaviour, the PGE are highly sensitive tracers of geological processes involving metal and sulfide phases.
-
The Critical Zone, October 2007, Vol. 3, No. 5
$20.00The Critical Zone (CZ) encompasses all fluid, mineral, gaseous, and biotic components from the outer envelope of vegetation down to the lower limit of groundwater. It supports much of life on Earth.
-
Frontiers In Textural And Microgeochemical Analysis, August 2007, Vol. 3, No. 4
$20.00Recent advances have been made in high-resolution in situ methods to image mineral growth patterns, analyse compositional and isotopic zonation, and improve our ability to visualize, study, and model rock textures in three dimensions. These advances provide a significant step forward in the understanding of how rocks form and the history they can tell us.
