Adiabats of quartz, coesite, olivine, and magnesium oxide to 50 kbar and 1000 K, and the adiabatic gradient in the Earth's mantle

Publisher： John Wiley & Sons Inc

E-ISSN： 2156-2202|87|B7|5501-5506

ISSN： 0148-0227

Source： Journal Of Geophysical Research, Vol.87, Iss.B7, 1982-07, pp. : 5501-5506

Disclaimer: Any content in publications that violate the sovereignty, the constitution or regulations of the PRC is not accepted or approved by CNPIEC.

Previous Menu Next

Abstract

Related content

The electrical conductivity of an isotropic olivine mantle

By  

Journal Of Geophysical Research, Vol. 97, Iss. B3, 1992-03 ,pp. : 3397-3404

John Wiley & Sons Inc

Access to resources Recommend Favorite

The quartz ⇆ coesite transformation: A precise determination and the effects of other components

By  

Journal Of Geophysical Research, Vol. 87, Iss. B8, 1982-08 ,pp. : 7073-7078

John Wiley & Sons Inc

Access to resources Recommend Favorite

High‐pressure infrared sepctra of ∝ ‐quartz, coesite, stishovite and silica glass

By  

Journal Of Geophysical Research, Vol. 98, Iss. B12, 1993-12 ,pp. : 22157-22170

John Wiley & Sons Inc

Access to resources Recommend Favorite

Thermodynamic properties of α‐quartz, coesite, and stishovite and equilibrium phase relations at high pressures and high temperatures

By  

Journal Of Geophysical Research, Vol. 100, Iss. B11, 1995-11 ,pp. : 22337-22347

John Wiley & Sons Inc

Access to resources Recommend Favorite

Lithospheric mantle thickness gradient focuses seismic activity

By  

Eos Transactions, Vol. 93, Iss. 39, 2012-09 ,pp. : 384-384

John Wiley & Sons Inc

Access to resources Recommend Favorite