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1
Course Presentation : ORGANIC GEOCHEMISTRY
Presented by
3.1. Gas Geochemistry
3.2.3. Derivation of liquids Oils dominantly from the Triassic Lacustrine mudstone 2
FOCUS OF MY PERSENTATION
Part # 1 : 3.1 Gas Geochemistry
Case study of Barbados Area
Characterized by Several major
gases in Barbados source rock
Thermal maturity interpretation
for gases
Biodegradation trends for gases
Sampling and methods
Conclusion
3
accretionary prism
Caribbean island, Barbados area
4
INTRODUCTION OF GAS GEOCHEMISTRY
Gas sampling,
storage, and
analysis
of gas samples
Important scientific
tool in constraining
processes occurring
in geosciences.
Quantitative
techniques: CO2 &
methane
migration(Climate)
Analytical
techniques :
Hydrocarbon, CO2,
N2, H2, CO and HG
vapour are
measured advance
method.
Hydrocarbon:
Isotopic Studies,
Gas
Chromatography
and Spectrometry.
CO2 & CH4, H2S and
HG vapour:
Seismotectonic and
biogeochemical
models
Gas sample from Thermal feature
Noble gases of Cosmo geochemistry
Volcanic Gas geochemistry Gas seepages sampling
5
CASE STUDY OF BARBADOS AREA
Cretaceous Marine Shale Deposit
Demonstrated petroleum systems: Minor oil & gas production, Several
oil seepages
Sample collection : Cutting & Core from Marine Shale outcrops
Geochemically define petroleum systems :
TOC(Total organic content ): <1 to 10 + weight percent.
HI (Hydrogen index) Rock _ Eval Pyrolysis : < 100 to 600+
Vitrinite reflectance analysis (%R < 0.6)
Tertiary Shale : oil window (0.6 – 1.4%), Gas Window(1.4 – 2.0%)
Study Area .(Hill and Schenk 2005)
Woodbourne Trough oil field 6
CHARACTERIZED BY SEVERAL MAJOR GASES IN
BARBADOS SOURCE ROCK
CO2
H2S
Methane
Ethane
Propane
n-butane
i-butane
n-pentane
i-pentane
7
Methane content :
ranges from 85 to
97 mol% with one
sample having a
value of 62%.
Carbon dioxide:
<0.60 mol% for all
samples
No H2S was
detected.
Methane carbon
isotope : - 38 to -
49‰.
Ethane from -32 to
- 35‰,
propane from K26
to K32‰
8
(Hill and Schenk 2005)
THERMAL MATURITY INTERPRETATION FOR GASES
Ranges of gas
thermal maturity
Gas mixtures
sampled collected
from sources
packages of
accretionary
prism
Fig. Carbon isotope plot for gas components, R0 = 0.7 and 1.0%
9
(Hill and Schenk 2005)
BIODEGRADATION TRENDS FOR GASES
Gas composition plot for thermal maturity and biodegradation trends.
10
(Hill and Schenk 2005)
METHODS
SAMPLING #
11
METHOD : GAS ANALYSIS
With flame ionization detector(FID), Thermal Conductivity detectors(TCD).
C1 – C5 hydrocarbon : Analysis using helium carrier gas, 2 Wasson KC5 columns & HP FID. Detection.
CO2, H2S, O2/Ar, N2 and CO non- hydrocarbon: Wasson K1 and K2S packed column & HP TCD.
Fig. Hewlett Packard(HP) 6890 GC by Wasson ECE Instrumentation
12
Fig. δ13C isotopic analysis for C1 – C4 and CO2 Gas
Micro mass Optima interfaced with a HP 6890 gas chromatograph: Pee Dee Belemnite Standard. 13
14
Part # 2: 3.2.3. Derivation of liquids Oils
dominantly from the Triassic Lacustrine mudstone
Case study of Tarim Basin
Samples & Methods
Hydrocarbons Discovered in kuqa depression
Crude oils classified in kuqa depression
Isotopic and biomarker interpretation for gases and
oils samples
Cross plots geochemically relationship groups of oil
& sources rocks
Conclusion
FOCUS OF MY PERSENTATION
15
CASE STUDY OF TARIM BASIN
Natural Gas, Condensate resources and small amount of black oil
High maturity level in Jurassic coal-bearing sequences : Peak stage of Dry gas generation
Sources rocks types: M- L- Jurassic coal-bearing with associated clastic and U- Triassic lacustrine
Mudstone : Stable carbon isotopes & Molecular Biomarker.
Triassic sources rock : Peak stage of oil generation occurred (early Miocene)
Gas and oil migrated : along fault relatively short lateral distance.
Traps formation : N to S margins and a late injection of gas into oil accumulation.
16
HYDROCARBONS DISCOVERED IN KUQA DEPRESSION
Bulk Carbon
isotopic values
ranges :
-24.6 to -31.6%.
Depletion 13C2
in Gas sample
13C2 values
ranges : -18.25
to -23.74%
>-24% : tighter
cluster
17
Table.1. showing the Stable carbon isotopes and pristine/phytane
ratio of oils, condensate, and oil seepages .
•Group .1 : Low δ13C(-27 to -31.6%) low pristine/phytane values(<2.5,
mostly <2.0)
•Group. 2 : High δ13C(-24 to -26.6%) High pristine/phytane
values(>2.5 )
Crude Oils
classified into two
genetic groups
CRUDE OILS CLASSIFIED IN KUQA DEPRESSION
18
Fig. δ13 C values for C1- C4 gaseous alkanes in the samples collected from the major gas fileds
ISOTOPIC AND BIOMARKER INTERPRETATION FOR GASES
AND OILS SAMPLES :
19
Table. Distribution of Jurassic and Triassic source rocks sample interpretation on the basis of Biomarker and Stable isotope
20
Secondary Classification criteria : Sterane & Terpane Distribution
Fig. Correlation of oil- condensate with potential sources rocks
Cross plots
Relationship
between the
two groups
of oils and
Source rocks
CROSS PLOTS GEOCHEMICALLY RELATIONSHIP GRPS OF
OIL & SOURCES ROCKS
21
Group 1 oils
Low in δ13C values, pristine/pythane & C24 tetracyclic/C26 Tricyclic terpane ratios but high C27 Steranes
22
Group 2 oils
Small reserves, Correlation with the extracts of Jurassic coal & mudstone
23
SAMPLES & METHODS
Gas samples : 13 oils & gas fields from Kuqa
Depression
Black oil : 5 samples
Condensate : 15 samples collected from 14 oil &
gas fields
Oil - Seepages : 3 samples
Oil- sand : 3 samples
Correlative based: 21 Mudstone & 19 Coal samples(
extraction with organic solvents Tr & Jr age)
24
METHODS
HP6890 Chromatograph fitted. MAT-252 mass spectrometer
25
Gas chromatography–mass spectrometry Vitrinite reflectance microscopy
26
27
28

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Oil and gas geochemistry

  • 1. 1 Course Presentation : ORGANIC GEOCHEMISTRY Presented by
  • 2. 3.1. Gas Geochemistry 3.2.3. Derivation of liquids Oils dominantly from the Triassic Lacustrine mudstone 2
  • 3. FOCUS OF MY PERSENTATION Part # 1 : 3.1 Gas Geochemistry Case study of Barbados Area Characterized by Several major gases in Barbados source rock Thermal maturity interpretation for gases Biodegradation trends for gases Sampling and methods Conclusion 3
  • 5. INTRODUCTION OF GAS GEOCHEMISTRY Gas sampling, storage, and analysis of gas samples Important scientific tool in constraining processes occurring in geosciences. Quantitative techniques: CO2 & methane migration(Climate) Analytical techniques : Hydrocarbon, CO2, N2, H2, CO and HG vapour are measured advance method. Hydrocarbon: Isotopic Studies, Gas Chromatography and Spectrometry. CO2 & CH4, H2S and HG vapour: Seismotectonic and biogeochemical models Gas sample from Thermal feature Noble gases of Cosmo geochemistry Volcanic Gas geochemistry Gas seepages sampling 5
  • 6. CASE STUDY OF BARBADOS AREA Cretaceous Marine Shale Deposit Demonstrated petroleum systems: Minor oil & gas production, Several oil seepages Sample collection : Cutting & Core from Marine Shale outcrops Geochemically define petroleum systems : TOC(Total organic content ): <1 to 10 + weight percent. HI (Hydrogen index) Rock _ Eval Pyrolysis : < 100 to 600+ Vitrinite reflectance analysis (%R < 0.6) Tertiary Shale : oil window (0.6 – 1.4%), Gas Window(1.4 – 2.0%) Study Area .(Hill and Schenk 2005) Woodbourne Trough oil field 6
  • 7. CHARACTERIZED BY SEVERAL MAJOR GASES IN BARBADOS SOURCE ROCK CO2 H2S Methane Ethane Propane n-butane i-butane n-pentane i-pentane 7
  • 8. Methane content : ranges from 85 to 97 mol% with one sample having a value of 62%. Carbon dioxide: <0.60 mol% for all samples No H2S was detected. Methane carbon isotope : - 38 to - 49‰. Ethane from -32 to - 35‰, propane from K26 to K32‰ 8 (Hill and Schenk 2005)
  • 9. THERMAL MATURITY INTERPRETATION FOR GASES Ranges of gas thermal maturity Gas mixtures sampled collected from sources packages of accretionary prism Fig. Carbon isotope plot for gas components, R0 = 0.7 and 1.0% 9 (Hill and Schenk 2005)
  • 10. BIODEGRADATION TRENDS FOR GASES Gas composition plot for thermal maturity and biodegradation trends. 10 (Hill and Schenk 2005)
  • 12. METHOD : GAS ANALYSIS With flame ionization detector(FID), Thermal Conductivity detectors(TCD). C1 – C5 hydrocarbon : Analysis using helium carrier gas, 2 Wasson KC5 columns & HP FID. Detection. CO2, H2S, O2/Ar, N2 and CO non- hydrocarbon: Wasson K1 and K2S packed column & HP TCD. Fig. Hewlett Packard(HP) 6890 GC by Wasson ECE Instrumentation 12
  • 13. Fig. δ13C isotopic analysis for C1 – C4 and CO2 Gas Micro mass Optima interfaced with a HP 6890 gas chromatograph: Pee Dee Belemnite Standard. 13
  • 14. 14
  • 15. Part # 2: 3.2.3. Derivation of liquids Oils dominantly from the Triassic Lacustrine mudstone Case study of Tarim Basin Samples & Methods Hydrocarbons Discovered in kuqa depression Crude oils classified in kuqa depression Isotopic and biomarker interpretation for gases and oils samples Cross plots geochemically relationship groups of oil & sources rocks Conclusion FOCUS OF MY PERSENTATION 15
  • 16. CASE STUDY OF TARIM BASIN Natural Gas, Condensate resources and small amount of black oil High maturity level in Jurassic coal-bearing sequences : Peak stage of Dry gas generation Sources rocks types: M- L- Jurassic coal-bearing with associated clastic and U- Triassic lacustrine Mudstone : Stable carbon isotopes & Molecular Biomarker. Triassic sources rock : Peak stage of oil generation occurred (early Miocene) Gas and oil migrated : along fault relatively short lateral distance. Traps formation : N to S margins and a late injection of gas into oil accumulation. 16
  • 17. HYDROCARBONS DISCOVERED IN KUQA DEPRESSION Bulk Carbon isotopic values ranges : -24.6 to -31.6%. Depletion 13C2 in Gas sample 13C2 values ranges : -18.25 to -23.74% >-24% : tighter cluster 17 Table.1. showing the Stable carbon isotopes and pristine/phytane ratio of oils, condensate, and oil seepages .
  • 18. •Group .1 : Low δ13C(-27 to -31.6%) low pristine/phytane values(<2.5, mostly <2.0) •Group. 2 : High δ13C(-24 to -26.6%) High pristine/phytane values(>2.5 ) Crude Oils classified into two genetic groups CRUDE OILS CLASSIFIED IN KUQA DEPRESSION 18
  • 19. Fig. δ13 C values for C1- C4 gaseous alkanes in the samples collected from the major gas fileds ISOTOPIC AND BIOMARKER INTERPRETATION FOR GASES AND OILS SAMPLES : 19
  • 20. Table. Distribution of Jurassic and Triassic source rocks sample interpretation on the basis of Biomarker and Stable isotope 20
  • 21. Secondary Classification criteria : Sterane & Terpane Distribution Fig. Correlation of oil- condensate with potential sources rocks Cross plots Relationship between the two groups of oils and Source rocks CROSS PLOTS GEOCHEMICALLY RELATIONSHIP GRPS OF OIL & SOURCES ROCKS 21
  • 22. Group 1 oils Low in δ13C values, pristine/pythane & C24 tetracyclic/C26 Tricyclic terpane ratios but high C27 Steranes 22
  • 23. Group 2 oils Small reserves, Correlation with the extracts of Jurassic coal & mudstone 23
  • 24. SAMPLES & METHODS Gas samples : 13 oils & gas fields from Kuqa Depression Black oil : 5 samples Condensate : 15 samples collected from 14 oil & gas fields Oil - Seepages : 3 samples Oil- sand : 3 samples Correlative based: 21 Mudstone & 19 Coal samples( extraction with organic solvents Tr & Jr age) 24
  • 25. METHODS HP6890 Chromatograph fitted. MAT-252 mass spectrometer 25
  • 26. Gas chromatography–mass spectrometry Vitrinite reflectance microscopy 26
  • 27. 27
  • 28. 28