TITLE:
Geochemical Study of Oil Shales Sargelo Formation in Kuh-e Kaino Section (Northern Masjed-Soleiman), Iran
AUTHORS:
Borzu Asgari Pirbalouti, Mahsa Moayeripour
KEYWORDS:
Geochemistry, Oil Shale, Sergalu Formation, Kuh-e Kaino, Kerogen
JOURNAL NAME:
Open Journal of Geology,
Vol.7 No.1,
January
20,
2017
ABSTRACT: Oil (bituminous) shales source rocks with variable amounts
of solid kerogen type II are the conditions for changing the oil that is not provided for them. Each of these shales affected in temperature
about 150 to 170 gallons of oil produced. Therefore by reducing hydrocarbon resources, it can be a good energy source for the future. To study the geochemistry of this shale, one section of outcrops in the Kuh-e Kaino (Northern Khozestan) was
selected which was located in the central Zagros. Chemical analysis and thin
sections were prepared from samples of carbonate shale. These deposits with a thickness of 115 m of the Lower Jurassic formations
Neyriz and Sargelo relative age and their relationship are gradual and interfinger. The upper border after
an erosional unconformity, Fahliyan Formation of Lower Cretaceous age on them covered. Analysis results show that the percentage of organic matter this shales in Kuh-e Kainois is equivalent to 8.44 percent. The index has gained economic value of metal elements Sr, V, Ba, Ni, and also has economic value. Bituminous materials formed stabilize in shaley
source rock of Sargelo formation, but not with continuous deposition on them, as a result of temperature and pressure
not increasing and immature kerogen. The causes of this event are as
follows: the basin tectonic condition, Stratigraphy position and faults
activity in the basin.