[HTML][HTML] Secular change and the onset of plate tectonics on Earth
The Earth as a planetary system has experienced significant change since its formation c.
4.54 Gyr ago. Some of these changes have been gradual, such as secular cooling of the …
4.54 Gyr ago. Some of these changes have been gradual, such as secular cooling of the …
Critical role of water in the formation of continental crust
Continental arcs are the sites of production of continental crust, but the origin of these
magmatic systems is not well understood. Although a number of processes have been …
magmatic systems is not well understood. Although a number of processes have been …
Collision of the North China and Yangtse Blocks and formation of coesite-bearing eclogites: timing and processes
Various types of eclogite, including coesite-bearing varieties formed under high-P-high-T
conditions (up to 27 kbar, 700–800° C), and glaucophane schist occur in the Dabie …
conditions (up to 27 kbar, 700–800° C), and glaucophane schist occur in the Dabie …
An experimental study of the effect of Ca upon garnet-clinopyroxene Fe-Mg exchange equilibria
DJ Ellis, DH Green - Contributions to Mineralogy and Petrology, 1979 - Springer
A series of basaltic compositions and compositions within the simple system CaO-MgO-FeO-
Al 2 O 3-SiO 2 have been crystallized to garnetclinopyroxene bearing mineral assemblages …
Al 2 O 3-SiO 2 have been crystallized to garnetclinopyroxene bearing mineral assemblages …
Lithospheric buoyancy and collisional orogenesis: Subduction of oceanic plateaus, continental margins, island arcs, spreading ridges, and seamounts
M Cloos - Geological Society of America Bulletin, 1993 - pubs.geoscienceworld.org
The sizes of continental blocks, basaltic oceanic plateaus, and island arcs that would cause
collisional orogenesis when they enter a subduction zone are calculated in an analysis …
collisional orogenesis when they enter a subduction zone are calculated in an analysis …
Partial melting of subducting oceanic crust
The conditions under which partial melting of subducting oceanic crust occurs can be
determined by combining a partial melting model for basaltic compositions with two …
determined by combining a partial melting model for basaltic compositions with two …
Eclogitization of lower crustal granulites by fluid migration through shear zones
H Austrheim - Earth and Planetary Science Letters, 1987 - Elsevier
The granulite facies assemblages of the anorthositic rocks of the Bergen Arcs (stable at 800–
900° C and 10 kbar) have been transformed to eclogite facies assemblages (stable at 700 …
900° C and 10 kbar) have been transformed to eclogite facies assemblages (stable at 700 …
High‐pressure granulites: formation, recovery of peak conditions and implications for tectonics
PJ O'Brien, J Rötzler - Journal of Metamorphic Geology, 2003 - Wiley Online Library
High‐pressure granulites are characterised by the key associations garnet‐clinopyroxene‐
plagioclase‐quartz (in basic rocks) and kyanite‐K‐feldspar (metapelites and felsic rocks) …
plagioclase‐quartz (in basic rocks) and kyanite‐K‐feldspar (metapelites and felsic rocks) …
[图书][B] Applied geothermics
L Eppelbaum, I Kutasov, A Pilchin - 2014 - Springer
Geothermics is an area of geophysics that studies the thermal state and history of the interior
of the Earth. Solar heat penetrates only into the topmost layers of the Earth's crust. Diurnal …
of the Earth. Solar heat penetrates only into the topmost layers of the Earth's crust. Diurnal …
Experimental phase-equilibrium study of Al-and Ti-contents of calcic amphibole in MORB—A semiquantitative thermobarometer
WG Ernst, J Liu - American mineralogist, 1998 - degruyter.com
Calcic amphiboles were synthesized from a natural mid-ocean ridge basalt (MORB) in 39
experiments representing 24 sets of pressure-temperature (PT) conditions ranging from 650 …
experiments representing 24 sets of pressure-temperature (PT) conditions ranging from 650 …