High temperature mineralization in the bituminous limestone in Maqarin area - north Jordan.

H. N. Khoury, S. Nassir

Research output: Contribution to journalArticle

29 Citations (Scopus)

Abstract

A high-T mineralization zone has been found in the bituminous limestone beds on the S bank of the Yarmouk River. The minerals include maghemite, hematite, gibbsite, gypsum, bassanite, diopside-hedenbergite and torbermorite. Spontaneous combustion of the organic matter was possibly responsible for the high T. In siliceous limestone this led to the formation of calcium silicates such as wollastonite, spurrite and anorthite. In the absence of silica, calcination of the limestone took place and highly alkaline waters enriched with Ca and OH formed portlandite, ettringite, thaumasite and baryte. Calcite and apatite were recrystallized by the high T.-I.Kb.

Original languageEnglish
Pages (from-to)197-213
Number of pages17
JournalNeues Jahrbuch fur Mineralogie, Abhandlungen
Volume144
Issue number2
Publication statusPublished - 1982

Fingerprint

Calcium Carbonate
limestone
mineralization
bassanite
hedenbergite
alkaline water
wollastonite
maghemite
anorthite
gibbsite
diopside
Spontaneous combustion
Calcium Sulfate
Banks (bodies of water)
Apatites
Temperature
hematite
gypsum
apatite
calcite

ASJC Scopus subject areas

  • Geochemistry and Petrology

Cite this

High temperature mineralization in the bituminous limestone in Maqarin area - north Jordan. / Khoury, H. N.; Nassir, S.

In: Neues Jahrbuch fur Mineralogie, Abhandlungen, Vol. 144, No. 2, 1982, p. 197-213.

Research output: Contribution to journalArticle

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