Hani Khoury

Prof. Hani Khoury

The University of Jordan
orcid

Research Focus & Metrics

Academic Career Length

48Years (1979-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 February 2015 in Applied Clay Science
Verified
Journal Article
Closed access
FAFaten Al-slaty
Faten Al-slaty
Hani KhouryHani Khoury
Hani Khoury
Hubert RahierHubert Rahier
Hubert Rahier
JWJan Wastiels
Jan Wastiels

15 June 2009 in Journal of Hazardous Materials
Verified
Journal Article
Closed access
RYRushdi Ibrahim Yousef
Rushdi Ibrahim Yousef
BEBassam EL-ESWED
Bassam EL-ESWED
Mazen AlshaaerMazen Alshaaer
Mazen Alshaaer
FKFawwaz Khalili
Fawwaz Khalili
Hani KhouryHani Khoury
Hani Khoury

1 May 2013 in Applied Clay Science
Verified
Journal Article
Closed access
FSFaten Slaty
Faten Slaty
Hani KhouryHani Khoury
Hani Khoury
JWJan Wastiels
Jan Wastiels
Hubert RahierHubert Rahier
Hubert Rahier

1 December 1981 in Facies
Verified
Journal Article
Closed access
PDF file
KBKlaus Bandel
Klaus Bandel
Hani KhouryHani Khoury
Hani Khoury

1 October 1982 in Clays and Clay Minerals
Verified
Journal Article
Closed access
Hani KhouryHani Khoury
Hani Khoury
DEDennis D. Eberl
Dennis D. Eberl
BJBlair F. Jones
Blair F. Jones
Deposits of sepiolite, trioctahedral smectite (mixed-layer kerolite/stevensite), calcite, and dolomite, found in the Amargosa Flat and Ash Meadows areas of the Amargosa Desert were formed by precipitation from nonsaline solutions. This mode of origin is indicated by crystal growth patterns, by the low Al content for the deposits, and by the absence of volcanoclastic textures. Evidence for low salinity is found in the isotopic compositions for the minerals, in the lack of abundant soluble salts in the deposits, and in the crystal habits of the dolomite. In addition, calculations show that modern spring water in the area can precipitate sepiolite, dolomite, and calcite following only minor evaporative concentration and equilibration with atmospheric CO2. However, precipitation of mixed-layer kerolite/stevensite may require a more saline environment. Mineral precipitation probably occurred during a pluvial period in shallow lakes or swamps fed by spring water from Paleozoic carbonate aquifers.

1 November 1992 in Journal of Geochemical Exploration
Verified
Journal Article
Closed access
Hani KhouryHani Khoury
Hani Khoury
ESE. Salameh
E. Salameh
ICI.D. Clark
I.D. Clark
PFP. Fritz
P. Fritz
WBW. Bajjali
W. Bajjali
WAW.R. Alexander
W.R. Alexander