Ann: Dunnart-2 Drilling Report No. 9, page-41

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  1. 3,530 Posts.
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    Be prepared for tomorrow - it's a gamble we all know that, if it does not play in our favour tomorrow find relief in this info from last Quarterly: map of Dunnart and related field and this very good reading

    Check the oil migration pathways on below map !

    ........
    EP437 EXPLORATIONAND PROSPECTIVITY REVIEW
    Exploration technical studies of the permit and surrounding area have been conducted in order
    to identify further prospects for drilling.
    The focus in the Perth Basin has been on shallow oil prospects that can be drilled with a small rig
    capable of drilling up to 1,000 metres and identifying a series of prospects that can be part of a
    targeted campaign after the 2014 exploration program.
    During the quarter it was announced that the
    Company was discussing a flexible five slot
    turnkey drilling contract with DCA for the use of
    Rig 7 from June 2014 to January 2015. This
    potential strategic agreement will provide for
    one firm well to be drilled with the option of four
    additional wells subject to approvals and
    financing.
    Exploration and appraisal wells (follow-up
    wells) currently identified include Dunnart-3
    and Wye Knot-1 in addition to a number of
    prospects including Condor South and up-dip
    Wattle Grove.
    The Wye Knot prospect is a three way dip
    closed anticline with a fault seal and is located
    approximately 10km west of the Mount Horner
    oilfield up-dip from the Dongara oil and gas
    field.
    Wye Knot-1 will target a best estimate prospective resource estimate of 5 million barrels2.
    The drilling of Wye Knot-1 would assess the Jurassic,
    Triassic and Permian oil objectives down-dip from the
    Wye-1 discovery well, which encountered gas in the
    Triassic Bookara sandstone (the same sandstone
    targeted in Dunnart-2) and gas in the Permian Wagina
    Sandstone. Good hydrocarbon shows were also
    encountered in the younger Jurassic sands and in the
    Aranoo sands within the Kockatea Shale.
    Very tight High Cliff to Nangetty sandstones below the
    base Kockatea were also penetrated in Wye-1. The
    seismic cross section from mapping (see next page)
    demonstrates the crossing of a fault into Early Permian
    sediments near basement. The tight nature of these
    sediments is likely due to the proximity to basement
    and exposure to silica rich fluids from basement in
    conjunction with high geothermal gradient on the
    Northampton Block to the north.
    2 As

 
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