J. Gittins et Re. Harmer, WHAT IS FERROCARBONATITE - A REVISED CLASSIFICATION, Journal of African earth sciences, and the Middle East, 25(1), 1997, pp. 159-168
The term ''ferrocarbonatite'' has been in use for about twenty years b
ut is not adequately defined. The IUGS system of igneous rock nomencla
ture defines it mineralogically as a carbonatite in which ''the main c
arbonate mineral is iron rich'' and chemically as a carbonatite in whi
ch (in weight percent) CaO:CaO + MgO + FeO + Fe2O3 + MnO < 0.8, and Mg
O < FeO + Fe2O3 + MnO. However, most rocks that have been called ferro
carbonatites do not have a high proportion of an Fe-rich carbonate min
eral and it is clear from their chemical analyses that most are calcit
e-hematite rocks or magnesian calcite-hematite rocks. Because the IUGS
system treats FeO, Fe2O3 and MnO as a single component it is unable t
o distinguish between calcite or dolomite carbonatites that contain he
matite or magnetite, and carbonatites that are composed largely of Fe-
rich ankerite, or of calcite and siderite. A modified chemical classif
ication is proposed using molar rather than weight proportions in whic
h the ferrocarbonatite field of the IUGS system is divided into two pa
rts so as to recognise a group of rocks to be known as ferruginous cal
ciocarbonatites, and to restrict the term ferrocarbonatite to much mor
e Fe-rich rocks. The revised classification is as follows: calciocarbo
natite: CCMF>0.75, magnesiocarbonatite: CCMF<0.75; MgO/FeO.>1.0, ferru
ginous calciocarbonatite: 0.5<CCMF<0.75;MgO/FeO.<1.0, ferrocarbonatite
: CCMF<0.5; MgO/FeO.<1.0 where CCMF is the molar ratio CaO/(CaO + MgO
+ FeO. + MnO) and FeO . refers to molar FeO if FeO and (FeO3)-O-2 are
both determined and total Fe as FeO if not. It is proposed that the te
rm ferrocarbonatite only be used in this modified chemical sense: carb
onatites in which the main carbonatite is I-e rich are adequately desc
ribed using the modal mineralogy. (C) 1997 Elsevier Science Limited.