【摘 要】
：
NaxK1-xAlSi3O8 hollandite(NaK-Holl)as a high pressure phase of feldspar is considered to be exist in subduction zones and to be a main phase carrying alkali elements in the mantle [1,2].
【机 构】
：
Key Laboratory of High-Temperature and High-Pressure Study of the Earth's Interior,Institute of Geo
【出 处】
：
第26届国际高压科学技术大会、第8届亚洲高压科技学术会议暨第19届中国高压科学技术会议(The 26th Interna
论文部分内容阅读
NaxK1-xAlSi3O8 hollandite(NaK-Holl)as a high pressure phase of feldspar is considered to be exist in subduction zones and to be a main phase carrying alkali elements in the mantle [1,2].
其他文献
Shock-induced opacity in Gd3Ga5O12(GGG)single crystals is investigated by transmission/emission measurements at 16 wavelengths(400-800 nm),as well as complementary particle velocity measurements at 15
The group-Ⅱ difluorides form materials with a variety of technological uses,and are analogues to several other AB2 compounds of industrial or geophysical significance,such as TiO2 and SiO2 [1,2].
Room-temperature superconductivity has been a long-held dream since 1911,and it is an area of intensive research.In 2004,Ashcroft shifted his attention to H-rich materials,which mimic the solid phases
Silicon borides are classical refractory materials because of their thermal stability.Recently,boron-doped silicon materials have attracted considerable attentions for their potential as promising sup
Using first-principles calculations,we predict a Chern insulating phase in thin films of the ferromagnetic semimetal GdN.In contrast to previously proposed Chern insulator candidates,which mostly rely
Heat flow conducted at the terrestrial planet outmost core is directly coupled to potential vigorous convection within the cores,generating magnetic field with different magnitudes [1].
Electromagnetic and seismic results from various subduction zones reveal that the presence of anomalies of electrical conductivity and seismic wave attenuation in the mantle wedge and fore-arc regions
Magnetotelluric(MT)study has become a powerful tool to detect the status of Earths interior.In order to explain the magnetotelluric data quantitatively,laboratory measurements on electrical conductivi
Phengite is a critical carrier of water and potassium in the sediment and the basalt layers of the subduction slab [1].
Previous works have measured the electrical conductivities of many minerals and rocks in the crust and upper mantle,and suggested interpretations of high-conductivity layers(HCLs)in the Earths interio