GrtBt&Facies4 0.3 0.0 1.2 1.5 0 400 200 600 800 1000 T emperature (°C) Pressure (GPa) eclogite granulite blueschist zeolite Prh- Pmp greenschist amphibolite Ep-Amp Sil And Ky wet granite melting Jd + QzAb ArgCc KASH PrlKy+Qz PrlAnd+Qz KyAnd KyAnd KySil Ms+QzSil+Kfs+L KFASH Hc+VFeCrd Alm+SilHc Alm+AlsFeCrd Ann+AlsFeCrd FeCrd+AnnAlm AlmAnn+Als StAlm+Als Cld+AlsSt CldAlm+Als AlmChl AlmAnn+Cld CldAlm+St AlmAnn+St StAnn+Als An+CldAlm FeChlAnn+Cld Ms+QzAls+Kfs+Bt KMASH Chl+AlsMgCrd PhlEn+MgCrd+Kfs+L Als+EnMgCrd Als+BtMgCrd Als+PhlMgCrd+Kfs+L LPhl+Kfs+V ChlAls+Bt ChlCrd+Bt KFMASH Als+BtGrt+Crd Grt+SilSpl+Crd ChlCrd+Bt+Sil CldSt+Grt+Bt Cld+ChlSt+Bt St+ChlCrd+Bt+Sil Cld+AlsSt+Chl Grt+Chl Cld+Bt Grt+ChlSt+Bt CldGrt+St+Chl Grt+ChlAls+Bt CldGrt+Als+Chl Grt+Cld+AlsSt Grt+Chl+Als St Grt+Bt+AlsSt Ms+QzAls+Kfs+Bt Ms+QzAls+Kfs+L Bt+GrtOpx+Als+L Bt+GrtOpx+Crd+Kfs+V LKfs+Grt+Crd+Bt+V Ms+VAls+L Bt+GrtOpx+Crd+L Opx+Als Grt+Crd Bt+AlsGrt+Crd+L Bt+AlsOpx+Crd+L Bt+GrtOpx+Als+L Bt+AlsGrt+Crd+L Opx+AlsGrt+Crd Bt+GrtOpx+Crd+V Ms+Ab+VAls+L Ms+AbAls+Kfs+L Bt+GrtOpx+Crd+L Bt+AlsOpx+Crd+L Grt+SilSpl+Crd Ms+AbAls+Kfs+V NaKFMASH


Show
Als Granite Facies
CcArg AbJdQz
KASH KFASH
KMASH KFMASH

Garnet-Biotite Mg-Fe
Exchange Coefficient (KD)


Garnet XMg (Mg/Fe)Grt

Biotite XMg (Mg/Fe)Bt


Grt-Bt Thermometer. Temperatures of metamorphosed shales using the compositions of garnet (Grt) and biotite (Bt) based on the experiments of Ferry and Spear (1978) and using equation 15-44 of Spear (1993) are shown with a rust-colored line. Move the sliders to change the KD values or the Grt and Bt compositions, or enter XMg (= Mg/(Mg+Fe) in moles) values into the boxes. Notice that pressure has little effect on the temperature for a given KD (the rust-colored line is nearly vertical).

Other reference reactions can be shown by clicking on the appropriate check boxes. Reactions for metamorphosed shale subsystems from the thermodynamic model dataset SPaC (version 4/2000) developed originally by Spear and Cheney (1989) may be shown by checking the boxes KASH, KFASH, KMASH, and KFMASH.