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Paper Number: 68
Deep
crustal CO2 fluxes in Jordan and their various geological
manifestations
Abu-Jaber, N.1
1Department
of Water and Environmental Engineering and Management, German Jordanian
University, Amman, Jordan, nizar.abujaber@gju.edu.jo
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Extensive recent investigations by the author of surfical vein
deposits, apparent caliche, crusts and other secondary carbonate
materials as well as groundwater have been conducted. These studies show
that the seepage has a profound effect on surface features,
geomorphology and groundwater quality. Moreover, a better understanding
of global CO2 fluxes can be achieved through the
quantification of deep sourced carbon which is possible through the
study of the Jordanian case.
In the Precambrian basement of southern Jordan, veins of carbonate
are growing within an alteration zone of rhyolite. The alteration and
the carbonate has been attributed to near surface geochemical processes
under ambient atmospheric conditions.
In the area of Petra in southern Jordan, extensive veins,
near-surface crusts, and pedogenic growths in loose surficial deposits
within the Palaeozoic sandstones have been linked to interaction of the
same deep sourced carbonate with entrapped water in near-surface
sediments and soils. Similar veins and crusts, in addition to other
alteration products have been studied in the Lower Cretaceous sandstones
of Wadi Kaniseh in central Jordan as well.
In the Upper Cretaceous limestone terrain of northern Jordan,
surfical deposits previously described as caliche are ubiquitous.
Preliminary investigations of their field relationships, petrography and
stable isotopic compositions suggest that these too may have been
deposited as a result of deep sourced carbon.
The deep groundwater aquifers in southern and central Jordan have
been highly influenced by carbon dioxide fluxes that have greatly
influenced the chemical quality of the water. The implications of this
discovery in terms of carbon capture and sequestration (CCS), water
quality, and geoarchaeology will be discussed.