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

H. N. Khoury, S. Nassir

نتاج البحث: المساهمة في مجلةمراجعة النظراء

34 اقتباسات (Scopus)

ملخص

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.

اللغة الأصليةEnglish
الصفحات (من إلى)197-213
عدد الصفحات17
دوريةNeues Jahrbuch fur Mineralogie, Abhandlungen
مستوى الصوت144
رقم الإصدار2
حالة النشرPublished - 1982
منشور خارجيًانعم

ASJC Scopus subject areas

  • ???subjectarea.asjc.1900.1906???

بصمة

أدرس بدقة موضوعات البحث “High temperature mineralization in the bituminous limestone in Maqarin area - north Jordan.'. فهما يشكلان معًا بصمة فريدة.

قم بذكر هذا