Ti in biotite and muscovite as an indication of metamorphic grade in almandine amphibolite facies rocks from Sudbury, Ontario

Details Ti in biotite and muscovite as an indication of metamorphic grade in almandine amphibolite facies rocks from Sudbury, Ontario Ti in biotite and muscovite as an indication of metamorphic grade in almandine amphibolite facies rocks from Sudbury, Ontario

Nov 1968

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1968gecoa..32.1222k&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 32, Issue 11, pp.1222-1229

Other

10

Scientific paper

Biotite and muscovite from rutile-bearing schists (almandine amphibolite facies) near Sudbury, Ontario, both show a linear increase of Ti content with increasing grade (475 to 725°C). In biotite, the increase of molar proportion of Ti from about 0·2 to 0·5 is accompanied by a linear decrease in content of the other main octahedrally-bound cations. The partition coefficient ( D Ti Biotite / Muscovite ) decreases 37 %.

Affiliated with

Also associated with

No associations

Rating

Ti in biotite and muscovite as an indication of metamorphic grade in almandine amphibolite facies rocks from Sudbury, Ontario does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Ti in biotite and muscovite as an indication of metamorphic grade in almandine amphibolite facies rocks from Sudbury, Ontario, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Ti in biotite and muscovite as an indication of metamorphic grade in almandine amphibolite facies rocks from Sudbury, Ontario will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1261384