Table 1 High-temperature minerals.

From: Evidence of Cosmic Impact at Abu Hureyra, Syria at the Younger Dryas Onset (~12.8 ka): High-temperature melting at >2200 °C

Phase

Formula

~Equilib Melt T (°C)

~Est. Flux Melt T (°C)

~Equilib Boil T (°C)

Est. O2 Fugacity (log)

Oxygen Fugacity Buffer

Chromite

(Fe)Cr2O4

2265

2065

2642

−14

Monazite

(Ce, La, Nd, Th)PO4

2072

1872

2230

Titanium sulfide

TiS

1780

1580

Zircon

ZrSiO4

1775

1575

2550

Chert

SiO2

1720

1520

2230

Quartz

SiO2

1720

1520

2230

Titano-magnetite

Fe2+(Fe3+, Ti)2O4

1625

1425

−3

Magnetite-hematite

Magnetite

Fe3O4

1590

1390

2623

−3

Magnetite-hematite

Wollastonite

CaSiO3

1540

1340

Hematite

Fe2O3

1538

1338

Magnetite-hematite

Chlorapatite

Ca5(PO4)3Cl

1530

1330

Nickel iron

NiFe

1430

1230

−12

Iron-wustite

Native iron

Fe

1420

1220

−12

Iron-wustite

Native Silicon

Si

1414

1214

Iron silicide

FeSi

1410

1210

−15

Titanium phosphide

TiP

1400

1200

Iron sulfide

FeS, Fe2S, Fe3S

1200

1000

Iron phosphide

Fe3P

1100

900

Ilmenite

FeTiO3

1050

850

  1. All minerals were observed on outer surfaces of AH glass or inner walls of vesicles. Laboratory heating experiments allow us to estimate flux-mediated melting points as ~200 °C below equilibrium melting points. Selected oxygen fugacities and respective buffers are shown.