Investigation of the paleodepositional environment of the Middle Miocene aged organic matter rich rocks (Tavas/Denizli/SW Turkey) by using biomarker parameters and stable isotope compositions (¹³C and ¹⁵N)

The study area is located 45 km south of Denizli. The purpose of this study is to identify the organic geochemical properties and paleo depositional environment of organic matter rich rocks from Tavas (Denizli/SW Turkey). For this purpose, total organic carbon (TOC, wt.%) and pyrolysis, n-alkane, is...

Full description

Bibliographic Details
Main Author: Demet Banu Koralay
Format: Article
Language:English
Published: General Directorate of Mineral Research and Exploration 2021-04-01
Series:Bulletin of the Mineral Research and Exploration
Subjects:
Online Access:https://dergipark.org.tr/tr/pub/bulletinofmre/issue/56453/742127
_version_ 1828029097660383232
author Demet Banu Koralay
author_facet Demet Banu Koralay
author_sort Demet Banu Koralay
collection DOAJ
description The study area is located 45 km south of Denizli. The purpose of this study is to identify the organic geochemical properties and paleo depositional environment of organic matter rich rocks from Tavas (Denizli/SW Turkey). For this purpose, total organic carbon (TOC, wt.%) and pyrolysis, n-alkane, isoprenoid, sterane, terpane and aromatic hydrocarbon parameters have been investigated of the studied samples. In addition, scanning electron microscopy (SEM) and stable isotope (δ¹³C and δ¹⁵N) investigations were also carried out. Organic matter rich rocks which have type III kerogen have got 25.80 and 44.00 wt.% TOC content. Hydrogen index (HI, 73 and 120 mg HC/g TOC) and Oxygen index (OI, 34 and 59 mg CO /g TOC) values of samples are very low. The values of δ¹³C and δ¹⁵N show the terrestrial C3 ecosystem. The predominance of high molecular weight n-alkanes, degree of waxiness and less dibenzothiophene (DBT) concentrations indicate terrestrial organic matter. At the same time, biomarker and pyrolysis parameters indicate that the organic matter rich rocks (Tavas/Denizli) are in the immature stage. Pr/Ph, C /C homohopane biomarker ratios and C35
first_indexed 2024-04-10T14:04:58Z
format Article
id doaj.art-f4c1355d749a42b183de62425ab0401a
institution Directory Open Access Journal
issn 0026-4563
language English
last_indexed 2024-04-10T14:04:58Z
publishDate 2021-04-01
publisher General Directorate of Mineral Research and Exploration
record_format Article
series Bulletin of the Mineral Research and Exploration
spelling doaj.art-f4c1355d749a42b183de62425ab0401a2023-02-15T16:10:04ZengGeneral Directorate of Mineral Research and ExplorationBulletin of the Mineral Research and Exploration0026-45632021-04-01164164395210.19111/bulletinofmre.74212776Investigation of the paleodepositional environment of the Middle Miocene aged organic matter rich rocks (Tavas/Denizli/SW Turkey) by using biomarker parameters and stable isotope compositions (¹³C and ¹⁵N)Demet Banu Koralay0Pamukkale University, Faculty of Engineering, Department of Geological Engineering, Denizli, TurkeyThe study area is located 45 km south of Denizli. The purpose of this study is to identify the organic geochemical properties and paleo depositional environment of organic matter rich rocks from Tavas (Denizli/SW Turkey). For this purpose, total organic carbon (TOC, wt.%) and pyrolysis, n-alkane, isoprenoid, sterane, terpane and aromatic hydrocarbon parameters have been investigated of the studied samples. In addition, scanning electron microscopy (SEM) and stable isotope (δ¹³C and δ¹⁵N) investigations were also carried out. Organic matter rich rocks which have type III kerogen have got 25.80 and 44.00 wt.% TOC content. Hydrogen index (HI, 73 and 120 mg HC/g TOC) and Oxygen index (OI, 34 and 59 mg CO /g TOC) values of samples are very low. The values of δ¹³C and δ¹⁵N show the terrestrial C3 ecosystem. The predominance of high molecular weight n-alkanes, degree of waxiness and less dibenzothiophene (DBT) concentrations indicate terrestrial organic matter. At the same time, biomarker and pyrolysis parameters indicate that the organic matter rich rocks (Tavas/Denizli) are in the immature stage. Pr/Ph, C /C homohopane biomarker ratios and C35https://dergipark.org.tr/tr/pub/bulletinofmre/issue/56453/742127tavas (denizli basin)organic geochemistrybiomarkersstable isotopes (¹³c nd ¹⁵n)depositional environment
spellingShingle Demet Banu Koralay
Investigation of the paleodepositional environment of the Middle Miocene aged organic matter rich rocks (Tavas/Denizli/SW Turkey) by using biomarker parameters and stable isotope compositions (¹³C and ¹⁵N)
Bulletin of the Mineral Research and Exploration
tavas (denizli basin)
organic geochemistry
biomarkers
stable isotopes (¹³c nd ¹⁵n)
depositional environment
title Investigation of the paleodepositional environment of the Middle Miocene aged organic matter rich rocks (Tavas/Denizli/SW Turkey) by using biomarker parameters and stable isotope compositions (¹³C and ¹⁵N)
title_full Investigation of the paleodepositional environment of the Middle Miocene aged organic matter rich rocks (Tavas/Denizli/SW Turkey) by using biomarker parameters and stable isotope compositions (¹³C and ¹⁵N)
title_fullStr Investigation of the paleodepositional environment of the Middle Miocene aged organic matter rich rocks (Tavas/Denizli/SW Turkey) by using biomarker parameters and stable isotope compositions (¹³C and ¹⁵N)
title_full_unstemmed Investigation of the paleodepositional environment of the Middle Miocene aged organic matter rich rocks (Tavas/Denizli/SW Turkey) by using biomarker parameters and stable isotope compositions (¹³C and ¹⁵N)
title_short Investigation of the paleodepositional environment of the Middle Miocene aged organic matter rich rocks (Tavas/Denizli/SW Turkey) by using biomarker parameters and stable isotope compositions (¹³C and ¹⁵N)
title_sort investigation of the paleodepositional environment of the middle miocene aged organic matter rich rocks tavas denizli sw turkey by using biomarker parameters and stable isotope compositions ¹³c and ¹⁵n
topic tavas (denizli basin)
organic geochemistry
biomarkers
stable isotopes (¹³c nd ¹⁵n)
depositional environment
url https://dergipark.org.tr/tr/pub/bulletinofmre/issue/56453/742127
work_keys_str_mv AT demetbanukoralay investigationofthepaleodepositionalenvironmentofthemiddlemioceneagedorganicmatterrichrockstavasdenizliswturkeybyusingbiomarkerparametersandstableisotopecompositions13cand15n