("Stellar Resources" or "the Company")
Update on Horse Hill discovery,
Update on Nutech well analysis - Further potential oil pay identified
Stellar Resources interest in Horse Hill:
The Horse Hill-1 well is located within onshore exploration license PEDL 137, on the northern side of the
Enquiries:
|
+44 (0) 20 7440 0640 |
James Caithie /
Public Relations: Square 1 |
+44 (0) 20 7148 7900
+44 (0) 20 7929 5599
|
UKOG news Release of
"The additional 250 geochemical analyses confirm that the HH-1 well penetrated a very thick section of world class, thermally mature, oil saturated source rocks in the Kimmeridge section encasing the Kimmeridge limestones and we look forward to receiving NUTECH's further rock sample analyses and the resultant final log interpretation in the coming few weeks."
"Of greatest note is that NUTECH's initial log analyses, utilising all the geochemical calibration points, strongly indicates that the Kimmeridge contains a potential oil pay section calculated from electric logs of over 300 feet with a further 73 feet of potential oil pay in the Oxford and Lias. The fact that the Kimmeridge potential pay section displays elevated electric log resistivity measurements within a sampled zone exceeding 2% TOC adds strength to NUTECH's interpretation."
"NUTECH's further lab analyses, specifically focussed to help calibrate electric log measurements of total porosity, are thus absolutely fundamental to provide the company with confirmation of the potentially significant oil-in-place contained in the well. The data and analyses to date give strong encouragement that the company has encountered something new and substantive in the Kimmeridge section of PEDL137 and PEDL246 to add to the HH-1
Update on HH-1:
Further to the announcement of
Geochemical results:
The results of the HH-1 detailed geochemical analysis confirm and conclude that the 1496 ft vertical thickness of Kimmeridge section in HH-1 contains three discrete thermally mature, highly organic rich, world class, claystone source rock units lying directly above, below and between the Upper and Lower Kimmeridge micritic limestone bands (see UKOG RNS
The new geochemical analyses demonstrate that an additional 140 feet thick, thermally mature, claystone source rock unit, exceeding 1% TOC, exists at the base of the Middle Jurassic Oxfordian to Cornbrash section from 5400-5540 ftmd. A distinct 50 foot section from 5450-5500 ftmd shows average metrics of 2.6% TOC, S2 of 16 Kg/tonne and an HI of 617. Furthermore a 60 foot thick section of the Lias from 7400-7460 ftmd exceeds 1% TOC, with average metrics of 1.5% TOC, S2 of 5 kg/tonne and HI of 443. More samples from this 60 foot Lias zone will be sent for additional RockEval pyrolysis.
Further geochemical analysis is planned in the well to understand the percentage of organic matter converted to hydrocarbons within all identified source units in the well together with values of initial TOC, S2 and HI prior to entering the hydrocarbon generative window
Thermal maturity:
As detailed in UKOG's
NUTECH Initial Log Analyses:
Since the
NUTECH's initial electric log analysis, utilising the 298 geochemical samples for calibration, indicates that in addition to the
The three Kimmeridge source units with TOCs above 2%, are interpreted by NUTECH to contain a total of 334 feet of net oil saturated potential pay. This interpreted Kimmeridge pay section demonstrates an elevated resistivity response compared to background non-source units of similar lithology.
An additional 43 feet of potential oil pay within a gross 90 foot interval is interpreted to exist within the claystones of the Middle Jurassic Oxford and Cornbrash section. A 30 foot potential pay zone in claystones is also calculated in the Lias, however, this interval has only two samples both demonstrating less than 2% TOC.
The geochemical and NUTECH initial log interpretation results are summarised in Table 1 below:
Table 1: Geochemical and NUTECH initial log analysis run
Formation Interval |
Gross Thickness >2% TOC |
NUTECH Net Oil zone |
Source Unit Measured TOC Weight % |
Generative Potential, S2 kg/tonne |
Hydrogen Index Kg H/tonne |
|||
Feet |
Feet |
Average |
Max |
Average |
Max |
Average |
Max |
|
Kimmeridge |
780 |
334 |
4.1 |
9.4 |
35 |
103 |
754 |
1000+ |
Oxfordian |
90 |
43 |
2.6 |
2.8 |
16 |
19 |
617 |
671 |
Lias |
- |
30 * |
1.5 |
1.6 |
5 |
6.5 |
443 |
445 |
Table 1: Geochemical and NUTECH initial log analysis run, source UKOG and NUTECH, *Calculated in a zone with 2 rock samples showing <2% TOC .
UKOG has a net attributable interest of 20.82% in the discovery
NUTECH Further Analysis:
NUTECH are currently running a further suite of 116 samples from 58 depth-points from the HH-1 for XRD (X-Ray Diffraction) and MICP (Mercury Injection Capillary Pressure) analysis in the US to provide more detailed calibration of the electric log response. These results are expected within the next few weeks. The final NUTECH evaluation of HH-1, with oil in place volumes per US sector (640 acres or square mile) is expected to be available shortly thereafter.
In addition, UKOG is working with NUTECH on their analyses of key wells surrounding the 140 km2 (34,600 acres) PEDL137 and PEDL246 licences to further define the likely semi-regional extent and size of the Kimmeridge, Oxford and Liassic oil bearing formations encountered in the HH-1 well. NUTECH will also research their extensive database of global producing oil wells to furnish UKOG with source and reservoir metrics from potentially analogous rock formations to the Kimmeridge.
UKOG's interest in Horse Hill:
The Horse Hill-1 well is located within onshore exploration License PEDL 137, on the northern side of the
Qualified Person's Statement:
For further information please contact:
UK Oil & Gas Investments PLC
David Lenigas /
WH Ireland (Nominated Adviser and Broker)
James Joyce / Mark Leonard Tel: 020 7220 1666
Square 1 Consulting (Public Relations)
David Bick / Mark Longson Tel: 020 7929 5599
Glossary: discovery |
a discovery is a petroleum accumulation for which one or several exploratory wells have established through testing, sampling and/or logging the existence of a significant quantity of potentially moveable hydrocarbons |
electric logs |
tools used within the wellbore to measure the rock and fluid properties of surrounding rock formations |
gamma-ray log |
an electric log which measures natural background radioactivity emitted mainly by potassium, uranium and thorium isotopes used as a sedimentary lithology discriminator |
generative potential (S2) |
the amount of hydrocarbons that can be generated from a unit volume of source rock established via the S2 peak from rock-evaluation pyrolysis, normally expressed in milligrammes of hydrocarbon per gramme of rock (or kilogramme per tonne). The S2 figure is achieved when 100% of the organic matter is transformed into hydrocarbons. |
hot shale |
a shale rock displaying average initial TOCs normally exceeding 2% and represented by a high gamma ray electric log reading |
hydrogen index (HI) |
the amount of hydrogen relative to the amount of organic carbon in a sample, normally expressed in milligrammes of hydrogen per gramme of TOC. The higher the amount of hydrogen the more oil prone the source rock when subjected to time temperature and pressure; an initial HI over 450 normally indicates an oil prone source rock |
measured depth |
The length of the wellbore, as if determined by a measuring stick. This measurement differs from the true vertical depth of the well in all but vertical wells. Since the wellbore cannot be physically measured from end to end, the lengths of individual joints of drill pipe, drill collars and other drill string elements are measured with a steel tape measure and added together. In virtually all cases, the actual wellbore is slightly deeper than the reported depth due to the expansion of the steel drill pipe under its own weight. |
MICP |
mercury injection capillary pressure. A technique to provide data for the calibration of porosity logs using fresh or archived cuttings samples as well as core. MICP analysis is performed by placing a tarred sample in the instrument chamber which is then evacuated and flooded with mercury. Pressure on the mercury is incrementally increased forcing mercury through progressively smaller pore throats. The volume of mercury forced into the sample is equivalent to the volume of porosity accessed. |
micrite |
a sedimentary rock formed of very fine grained calcareous particles ranging in diameter from 0.06 to 2 mm, often referred to as lime mudstone |
pay |
A reservoir or portion of a reservoir that contains economically producible hydrocarbons. The term derives from the fact that it is capable of "paying" an income. The overall interval in which pay sections occur is the gross pay; the smaller portions of the gross pay that meet local criteria for pay (such as minimum porosity, permeability and hydrocarbon saturation) are net pay. |
oil initially in place |
the quantity of oil or petroleum that is estimated to exist originally in naturally occurring accumulations before any extraction or production |
oil saturation |
the amount of the pore space within a reservoir containing oil |
play |
a set of known or postulated oil and or gas accumulations sharing similar geologic, geographic, and temporal properties, such as source rock, migration pathways, timing, trapping mechanism, and hydrocarbon type |
porosity |
the percentage of void space in a rock formation, where the void may contain, for example, water or petroleum |
pyrolysis |
pyrolysis is the decomposition of organic matter by heating in the absence of oxygen. Organic geochemists use pyrolysis to measure TOC, generative potential (S2), richness (HI) and maturity of potential source rocks. In a pyrolysis analysis, the organic content is pyrolyzed in the absence of oxygen, then combusted. The amount of hydrocarbons and carbon dioxide released is measured. |
reservoir |
a subsurface rock formation containing an individual natural accumulation of moveable petroleum that is confined by impermeable rock/formations |
RockEval |
the most widely used pyrolysis technique. |
source rock |
a rock rich in organic matter which, if subjected to sufficient heat and pressure over geological time, will generate oil or gas. Typical source rocks, usually shale or limestone, contain above an initial 1% organic matter by weight |
sweet spot |
the area within a shale source rock unit showing highest TOC and generative potential normally associated with basin centred deposition |
thermally mature |
a term applied to source rocks which have received sufficient temperature and pressure over geological time to generate hydrocarbons |
TOC |
total organic carbon - the weight percent amount of organic carbon within the rock which is a commonly used measure of hydrocarbon source rock richness |
tvdss |
true vertical depth below a subsea datum |
vitrinite reflectance (Ro) |
a measure of the percentage of incident light reflected from the surface of vitrinite particles in a sedimentary rock. It is referred to as % Ro and is a measure of the thermal maturity of a rock. Top of the oil window is dependent on source rock type, but is widely recognized to be at an Ro equivalent of between 0.5-0.6% |
XRD |
X-ray diffraction. A technique used to determine the precise mineralogical content of a rock sample |
This information is provided by RNS