WEST OF SCOTLAND
Thermal and tectonic development
and hydrocarbon generation history assessed using AFTA® and
vitrinite reflectance
NON-EXCLUSIVE
PROJECT
1. INTRODUCTION
Geotrack initiated
the West of Scotland project in May 1995 to acquire the thermal history
data needed to recognise and characterise the thermal episodes that
have affected the region, and assess the development of maturity, hydrocarbon
generation and tectonic evolution. The data produced by the project
are critical to understanding and predicting oil and gas generation
in the region.
The project is
based on 124 AFTA and 128 vitrinite reflectance samples from 11 wells
and 39 offshore shallow boreholes from the Malin, Hebrides, Minch, West
Orkney and Outer Hebrides regions and from outcrop locations in the
Hebridean Isles, Skye, Mull and the Scottish mainland. The project has
been funded by several groups of oil companies and includes data and
analyses of samples from four non-released wells provided by supporting
companies. Relevant data from recently completed studies in adjacent
areas in the North Channel and West of Shetlands are integrated with
the new data to provide continuous thermal history data coverage along
the Western margin of the UK continental shelf.
The final report
presents all the AFTA and VR data and a rigorous interpretation of thermal
history and its effects on maturity development and hydrocarbon generation,
providing the maximum amount of hard data on thermal history of the
region that modern methods allow. The report can be purchased on a non-exclusive
basis. This document provides background to the project, details of
the database and prices.
2. BACKGROUND
TO THE PROJECT
The onshore and
offshore basins north and west of Scotland represent over 100,000km2
of the UK continental shelf that is virtually unexplored by drilling.
The region contains a complex of basins containing Permian, Triassic
and Jurassic sequences. Onshore, the Jurassic contains thick source
rock sections and oil stained sandstones. Source rocks also occur in
the Upper Carboniferous section at outcrop, which can be inferred to
underlie large parts of the region.
Hydrocarbon prospects
depend critically on the thermal history and its control on maturity
development and hydrocarbon generation through the history of these
basins. Prospectivity also depends on the tectonic evolution, particularly
the history of uplift and erosion with its consequent effects on source
rock maturation and reservoir distribution.
AFTA studies of
adjacent regions in the Irish Sea, North Channel and West of Shetlands
have revealed complex thermal histories. Several episodes of heating
and cooling have affected the Upper Paleozoic and Mesozoic sections.
In the Irish Sea for example, known hydrocarbon accumulations are restricted
to those areas where paleothermal episodes late in the history dominate
the maturation of Carboniferous source rocks. The West of Scotland region
has possible analogies with the Irish Sea, both in the potential for
Carboniferous source rocks and the in the possibility of dominant paleothermal
episodes late in the history linked with igneous activity. Potential
analogues also exist in the West of Shetlands region, where paleothermal
episodes affecting the Jurassic source rocks show complex but consistent
patterns.
This project sets
out to link the thermal history data from the wells in the southern
part of the West of Shetlands area through the Outer Hebrides Shelf
and Western Isles into Northern Ireland and the North Channel, hence
filling a large gap in our knowledge of the thermal and tectonic evolution
of the UK western continental shelf.
3. STUDY OBJECTIVES
The primary study objectives are
to:
- Apply AFTA and VR data to recognise
the dominant paleothermal episodes and identify their geological timing
and geographical distribution.
- Reconstruct paleotemperature
profiles and determine paleo- geothermal gradients from vertical sequences
of AFTA and VR samples in wells, and evaluate to help establish the
origins and mechanisms of the heating.
- Determine maximum and peak paleotemperatures
and their geological timing. Establish a regional thermal history
framework within which the history of hydrocarbon generation can be
understood.
- Assess levels of maturity in
Jurassic and Carboniferous source rocks and determine when this maturity
was developed.
- Assess the effects of the Tertiary
igneous activity, including localised heating; widespread effects
due to convection and fluid flow, possible associated high basal heat
flow.
- Identify the timing of the significant
phases of uplift and erosion; estimate the amount of eroded section;
assess the significance
- Produce a regional synthesis
of thermal history, maturity development and hydrocarbon history.
4. AFTA AND VR
DATA AND SAMPLE DETAILS
AFTA data have
been acquired and processed to the highest industry standard by Geotrack
International. Apatite yields from the samples analysed are generally
good to excellent resulting in high data quality. Data interpretation
has been carried out using Geotrack's recently introduced multi compositional
apatite annealing model which makes rigorous allowance for the controls
of apatite composition on annealing rates. This includes microprobe
analysis of all apatite grains and compilation of chlorine content data
for each sample. In wells 134/5-1 and IR 12/13-1 where pre-existing
AFTA data are being used, the data have been re-evaluated using the
multi compositional model and the most up-to-date interpretation system.
The vitrinite reflectance
data has been acquired to a high standard by Prof. Alan Cook, widely
regarded as one of the most experienced analysts currently practising.
The data have been produced using the exacting Romax
method, in common with other Geotrack studies. The VR data are presented
with full organic maceral descriptions and data histograms.
The number of samples
taken for AFTA and VR for each stratigraphic unit are shown below in
brackets. Contact us for the location of wells, shallow boreholes and
outcrop samples.
EXPLORATION WELLS:
132/15-1 IR 12/13-1
AFTA - Tertiary (5), Archaean
(1) AFTA - Cretaceous (3), Triassic (3)
VR - Tertiary (14) VR - Tertiary
(2), Cretaceous (3), Jurassic (1), Triassic (5)
134/5-1 IR 13/3-1
AFTA - Jurassic (3), Triassic
(5) AFTA - Carboniferous (4), Igneous rock (1)
VR - Jurassic (26), Triassic
(3) VR - Carboniferous (16)
156/17-1 202/19-1
AFTA - Triassic (4), Torridonian
(1) AFTA - Permo-Triassic (9)
VR - Jurassic (5)
164/25-1 Port More-1
AFTA - Permo-Triassic (3), Tertiary
(10) AFTA - Triassic (4)
VR - Tertiary (16), Cretaceous
(7) VR - Jurassic (4)
164/25-2 Magilligan-1
AFTA - Tertiary (5), Archaean
(1) AFTA - Triassic (2), Carboniferous (1)
VR - Tertiary (10) VR - Jurassic
(1), Triassic (1), Carboniferous (5)
SHALLOW BOREHOLE AND SEA BED
CORE SAMPLES:
AFTA: VR:
BH71/09 Devonian BH72/33 Jurassic
BH71/10 Jurassic BH76/55 Jurassic
BH71/11 Permo-Triassic BH78/02
Jurassic
BH71/12 Jurassic BH78/04 Jurassic
BH71/13 Torridonian BH85/08 Jurassic
BH71/14 Permo-Triassic
BH72/32 Permo-Triassic
BH78/02 Jurassic
BH78/05 Triassic
BH81/12 Permo-Triassic
BH81/13 Triassic?
BH88/04 Triassic
BH88/08 Triassic
BH90/08 Permo-Triassic
BH90/09 Permo-Triassic
BH90/12A Permo-Triassic
BH90/14 Lewisian
BH90/16 Triassic
94 Permo-Triassic
642 Jurassic
666 Tertiary?
OUTCROP SAMPLES
AFTA:
Jurassic (9)
Lewisian (6) Cretaceous (2)
Torridonian (4) Tertiary (4)
Dalradian and Moine (6)
Devonian (2)
VR:
Carboniferous (2) Jurassic (7)
Permo-Triassic (3) Carboniferous
(1)
For further details
please contact us