Hydrous Phases and Hydrogen Bonding at High Pressure

Research Article| January 01, 2000 Hydrous Phases and Hydrogen Bonding at High Pressure Charles T. Prewitt; Charles T. Prewitt Geophysical Laboratory and Center for High Pressure Research, Carnegie Institution of Washington, 5251 Broad Branch Road, NW, Washington, DC 20015 Search for other works by this author on: GSW Google Scholar John B. Parise John B. Parise Department of Geosciences and Center for High Pressure Research, State University of New York at Stony Brook, Stony Brook, New York 11794 Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2000) 41 (1): 309–333. https://doi.org/10.2138/rmg.2000.41.11 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Charles T. Prewitt, John B. Parise; Hydrous Phases and Hydrogen Bonding at High Pressure. Reviews in Mineralogy and Geochemistry 2000;; 41 (1): 309–333. doi: https://doi.org/10.2138/rmg.2000.41.11 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Hydrogen is the simplest and most abundant element in the universe. It is the third most abundant element on the surface of the planet. Studies and interpretation of the spectroscopic properties of hydrogen, and those of its isotopes, have been intertwined with the development of experimental and theoretical physics and chemistry. It is now realized that hydrogen forms more chemical compounds than any other element, including carbon, and a survey of its chemistry would encompass the whole periodic table. In mineralogy hydrogen is also ubiquitous. The range of minerals capable of hosting hydrogen range from ice to nominally anhydrous silicate... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.