RB 2020/00022 Delamerian igneous basement to the Murray Basin in South Australia: a drill core review - volume 1.
Published: 01 Aug 2020 Created: 15 Nov 2024 Revised: 13 Jan 2025

This report presents the results of a Geological Survey of South Australia drillhole core samples logging project addressing a selection of the cored historical exploration and stratigraphic holes that have penetrated probable Delamerian Orogeny...

This report presents the results of a Geological Survey of South Australia drillhole core samples logging project addressing a selection of the cored historical exploration and stratigraphic holes that have penetrated probable Delamerian Orogeny - age igneous and volcano-sedimentary basement to the Murray Basin in South Australia. It also includes a small number of holes from the eastern range front of the Flinders Ranges, which it was thought might be illustrative of concealed basement in the north-western Murray Basin, where few cored holes exist. The contents of this report are intended to be descriptive rather than interpretative, providing the foundation for further analytical work to be done on the drill cores, such as geochronology and geochemistry, which will be necessary to develop a stratigraphy and characterise the magmatic history of this part of the Delamerian Orogen. The holes were selected based on the information provided in lithological and stratigraphic logs available in SARIG, with the objective of including holes with a broad geographic spread which contain a diverse range of lithologies. There are, however, many cored holes that have penetrated igneous or volcano-sedimentary basement which have not been included. The 95 cored holes described herein were re-logged at the DME Tonsley Core Library during the period October 2018 to July 2020. Only the basement intervals in the holes were logged, which total over 6000 m in length. The descriptions of the cores are supported by thin section petrography, including that for 47 new thin sections collected as part of this study, plus results of the re-examination of 210 thin sections previously collected from these drillholes and stored within the GSSA thin section collection at Tonsley. Existing petrology report findings relating to the logged drillholes, contained within exploration company dataset envelopes and generated by petrography studies done as part of the Murray Basin Basement Transect Project (Farrand, 1991; Farrand & Rankin, 1991; Farrand, 1992), were incorporated into the lithological descriptions accompanying the logs. The study has been structured into five regions, (i) North-western Murray Basin margin, (ii) Truro - Cambrai, (iii) Far West, (iv) Karoonda - Coonalpyn and (v) Tintinara - Padthaway, although no geological significance is implied by these divisions. This volume contains the logs for drillholes from the North-western Murray Basin margin, Truro - Cambrai, Far West and Tintinara - Padthaway regions; the logs for drillholes from the Karoonda - Coonalpyn region will be presented in a second volume (Curtis, in prep.). A graphic lithological log is presented for each hole (except those holes with less than 1 m of core), accompanied by a description of the main lithologies, contact relationships, deformational fabrics, alteration and mineralisation. The level of detail provided in the descriptions is variable between drillholes, being largely dependent on the complexity of the rocks and the amount of petrology information available. The majority of the logs are presented at a scale of 1:100 or 1:200, but a small number are presented at a scale of 1:10 or 1:400 depending on hole length and lithological complexity. The grain size on the lithology logs is taken as the coarsest mineral phase, not the dominant grain size. A legend to the graphic logs is provided in a separate figure (Fig. 3). The cored basement depths, major lithologies, secondary mineralogy (which includes metamorphic and alteration minerals) and structural fabrics for the drillholes from each region are summarised in Tables 1–4.

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About this record

Record No 2020d032474
Topic Geoscientific Information
Type of Resource Document
Category Type
Document Type Departmental Publication - Geological Survey Geoscience Publication
Contributor Geological Survey of South Australia;South Australia’s 4D Geodynamic and Metallogenic Evolution Team;Geoscientific Information Strategy Team
Sponsor
Tenement
Tenement Holder
Operator
Geological Province
Mine Name
Stratigraphy
Commodity
    Notes
    Notes: This drill core review forms part of the Phase 1 data release for the MinEx CRC Delamerian NDI Project.   The Adelaide Fold Belt in the far western part of the Delamerian Orogen consists of Neoproterozoic and Early–Middle Cambrian...

    Notes: This drill core review forms part of the Phase 1 data release for the MinEx CRC Delamerian NDI Project. The Adelaide Fold Belt in the far western part of the Delamerian Orogen consists of Neoproterozoic and Early–Middle Cambrian sedimentary rocks and syn-orogenic felsic and mafic intrusive rocks that were thrust back onto the continental margin during the c. 514–490 Ma Delamerian Orogeny (Flöttmann et al. 1994; Foden et al. 2006), the collisional event that terminated subduction (Cayley, 2011). The Grampians - Stavely Zone and Glenelg River Zone in Victoria and the Koonenberry Belt and Loch Lily - Kars Belt in New South Wales, in the far eastern part of the orogen, contain igneous rocks with volcanic arc affinities, and are interpreted to have formed within the volcanic arc and back arc of the subduction system (Kemp, 2001, Sharp et al. 2006; Greenfield et al. 2010, Schoefield et al. 2018). However, the nature of the Delamerian basement in the intervening area, beneath the western Murray Basin in South Australia, is poorly understood, and is currently the focus of a major project by the Geological Survey of South Australia, as part of the MinEx CRC National Drilling Initiative (Curtis and Wise, 2019). The basement to the Murray Basin in South Australia is known only from a small number of outcrops in the Padthaway Ridge region in the far south-west of the basin (Turner et al. 1992), and from exploration and stratigraphic drilling. A number of major basement exploration programs were carried out in the Murray Basin in the late 1970s to early 2000s, most notably by North Broken Hill Ltd (Envelope 02631), Thiess Brothers (Envelopes 03316 and 03317), C.R.A. Exploration (Envelope 03957), C.S.R. (Envelope 04719), Pasminco Exploration (Envelopes 08941, 08947, 09014, 09015, 09016 and 09130) and Normandy Gold Exploration (Envelopes 09568, 09721 and 09739). More recent programs in this region have included those by Red Metal Ltd (Envelope 11492), Gold Fields Australasia (Envelopes 12175 and 11448), and Seesaw Resources (Envelope 13048). This exploratory drilling is, however, restricted almost entirely to a narrow belt lying within 50 km of the western edge of the Murray Basin, where cover thickness is perceived to be shallowest. Within the basin proper, the most significant basement exploratory drilling was done by the Geological Survey of South Australia in the 1990s, as part of the Murray Basin Basement Transect Project (Rankin et al. 1991). In addition, a number of water bores drilled in this region have provided valuable information about basement (Ludbrook, 1959; Preiss and Radke, 1989; Gatehouse et al. 1991). Geographic Locality: South Australia;Manunda;Kia Ora;Canegrass;Murray Mallee;Peebinga;Lameroo;Truro;Cambrai;Blanchetown;Upper South-East;Tintinara;Keith;Padthaway;Kingston S.E. Doc No: RB 2020/00022 Drillhole: 82FNSRM1;(87125);AH DDH4 - AH DDH6;(104020 -104022);AN DDH1 - AN DDH3;(103960 - 103962);BD1;(77469);BD4;(77623);BD5;(77483);DDH AN7;(144355);M154 / NANYAH 1;(103816);PADD35;(185026);83FS61RM1;(86637);83FS34RM1;(77125);83FS84RM1;(252772);BLACK HILL 1;(184147);DEL10ACD001;(261383);DEL10ACD346 - DEL12ACD349;(271558 -271560);PADD005;(186200);PADD011 - PADD013;(186206 - 186208);PADD016;(186211);SAW001;(294568);SAW002;(294569);MBT1 / PEEBINGA 1;(126805);MBT5 / WIRHA SOUTH 1;(186237);MBT6 / TORI HILLS 1;(102447);CODD1;(186234);CODD4;CODD5;(186238);KEITH 1;(122487);KIN5;(158331);KTH1 - KTH5;(167571 - 167575);KTH11;(167585);KTH 12;(167586);LD3;(169146);MTR3;(174039);MTR5;(174041);MTR7;(174043);PADD029;(186224);PADD030;(186225);TN1a;(151503)

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    Language English
    Metadata Standard ISO 19115-3

    Citations

    Use constraints License
    License Creative Commons Attribution 4.0
    Persistent identifier https://pid.sarig.sa.gov.au/document/2020d032474
    Citation Curtis, S.O. 2020. RB 2020/00022 Delamerian igneous basement to the Murray Basin in South Australia: a drill core review - volume 1. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
    https://pid.sarig.sa.gov.au/document/2020d032474

    Technical information

    Status
    Maintenance and Update Frequency
    Geographic Reference GDA2020 (EPSG:7844)
    Geo bounding box {"type":"Polygon","coordinates":[[[139,-36],[139.5,-36],[139.5,-32],[139,-32],[139,-36]]]}
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