Newly recognized occurrences of ultrahigh-pressure (UHP) minerals including diamonds in
ultrahigh-temperature (UHT) felsic granulites of orogenic belts, in chromitites associated with …

A pyrope-quartzite originally described by Vialon (1966) from the Dora Maira massif was
resampled and reinvestigated. Garnet (up to 25 cm in size), phengite, kyanite, talc and rutile …

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 …

Coesite is reported for the first time from the Caledonide orogen. It occurs as inclusions in
clinopyroxene in the dolomite-eclogite at Grytting, Norway, and provides valuable new …

The idea for a book on anorthosites came to me in January of 1986 while returning to
Houston after holiday festivities in Dallas. The original idea was a review paper on …

Coesite and Coesite pseudomorphs are recognized in eclogite from the Dabie Mountains, a
collision zone between the Sino-Korean and Yangtze cratons in central China. This third …

In these days of information explosion and high-cost publishing, it is perhaps only
reasonable for an author to convince the reading public that it is getting something worth …

Diamonds and other ultrahigh pressure (UHP) minerals have been reported previously from
the Luobusa ophiolite of Tibet, but these minerals have thus far been found only as …

We present new experimentally determined trace element partition coefficients for nine
garnet/melt and two clinopyroxene/melt pairs at 2.9–3.1 GPa and 1325°–1390° C …

The discovery of coesite (Chopin 1984, Smith 1984) and microdiamonds (Sobolev and
Shatsky 1990) in very high-pressure (VHP) 1 crustal rocks is revolutionizing our …