<?xml version="1.0" encoding="UTF-8"?><rss xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:content="http://purl.org/rss/1.0/modules/content/" xmlns:atom="http://www.w3.org/2005/Atom" version="2.0"><channel><title><![CDATA[Caadia]]></title><description><![CDATA[At CAADIA Metals, we believe the next generation of mineral deposits in Australia will be discovered through data intelligence.]]></description><link>https://www.caadiametals.com.au/project-summaries</link><generator>RSS for Node</generator><lastBuildDate>Fri, 24 Jul 2026 03:17:21 GMT</lastBuildDate><atom:link href="https://www.caadiametals.com.au/blog-feed.xml" rel="self" type="application/rss+xml"/><item><title><![CDATA[Dowling–Koorabri ]]></title><description><![CDATA[Geological setting and mineral system The prospect occupies the Goodradigbee Graben between the Cowra Trough and the Cotter Horst, where the Koorabri Fault — a splay of the first-order Long Plain Fault — juxtaposes Lower Silurian limestone–chert–shale sediments against the Lower Devonian Mountain Creek Volcanics (Quek 1980a, R00016067). A calc-silicate corridor (clinopyroxene–garnet–epidote–actinolite, locally barite-bearing) of ~3–5 km strike and up to ~80 m apparent (outcrop) width — true...]]></description><link>https://www.caadiametals.com.au/post/dowling-koorabri</link><guid isPermaLink="false">6a61ea3121af5c246d00dca0</guid><category><![CDATA[Woodlawn / Captains Flat belt]]></category><pubDate>Thu, 23 Jul 2026 10:19:34 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_5dc28c92dd8b41809be4e15e1f6c58e6~mv2.png/v1/fit/w_755,h_479,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Bungendore Corridor]]></title><description><![CDATA[Geological setting and mineral system Two prospects, one tenement application, on the Silurian volcano-sedimentary belt of the Captains Flat–Goulburn Synclinorial Zone, eastern Lachlan Orogen — the belt hosting the Woodlawn and Captains Flat Cu–Pb–Zn–Ag VMS deposits (R00005792). At Clare, gossans with box-work after sulphides sit at a sediment–volcanic contact with a footwall limestone in CD2; the NSW Department of Mines assessing geologist (L. A. Gilligan, 9 September 1974) characterised the...]]></description><link>https://www.caadiametals.com.au/post/bungendore-corridor</link><guid isPermaLink="false">6a61e8af59dc3f2805c1f95f</guid><category><![CDATA[Woodlawn / Captains Flat belt]]></category><pubDate>Thu, 23 Jul 2026 10:14:07 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_53a46c1e86b04ef9b065eaedb3b123b1~mv2.png/v1/fit/w_836,h_671,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Talagandra]]></title><description><![CDATA[Geological setting and mineral system The three prospects sit in a fault-bounded Silurian volcanic–sedimentary basin of the eastern Lachlan Orogen, hosted by the same lithostratigraphic package (Westmead Park Formation of Smith 1965, equivalent to Canberra Formation unit Smc of Abell 1992), on the belt that hosts Woodlawn and Captains Flat in correlative Silurian stratigraphy (Nisbet 1979, GS1979/129, R00015991). Two complementary deposit-style models are supported by the evidence and are not...]]></description><link>https://www.caadiametals.com.au/post/talagandra</link><guid isPermaLink="false">6a61e51e424f5a9980a43285</guid><category><![CDATA[Woodlawn / Captains Flat belt]]></category><pubDate>Thu, 23 Jul 2026 09:58:55 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_a34c09e0b4334c489179a05c1529d53b~mv2.png/v1/fit/w_929,h_551,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Border Downs]]></title><description><![CDATA[Geological setting and mineral system The target sits at the Curnamona Province – Delamerian Orogen boundary within the outcrop-poor Thomson cover region, beneath approximately 442 m of Eromanga/Darling Basin cover; basement is interpreted as probable Middle to Late Neoproterozoic quartz-rich shallow-marine clastics (R00036180). The intersection is recorded in GSNSW MinView as MIN_043525 (drill type Other — water bore; business purpose metallic minerals), with the mineralisation documented by...]]></description><link>https://www.caadiametals.com.au/post/border-downs</link><guid isPermaLink="false">6a61e24959dc3f2805c1e465</guid><category><![CDATA[Western NSW]]></category><pubDate>Thu, 23 Jul 2026 09:46:07 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_47d4b27128b44ff3af786e73daba330a~mv2.png/v1/fit/w_841,h_526,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Coopers-Curraba]]></title><description><![CDATA[Geological setting and mineral system The prospect sits in the Woolomin Beds of the southern New England Orogen — polydeformed, highly siliceous metasediments with green schists, jaspers, cherts and tuffaceous interbeds — a belt that hosts structurally controlled orogenic gold and antimony–gold mineralisation elsewhere (R00029633; R00029598). The State metallogenic record already classifies the deposit as a gold system: the Tamworth–Hastings 1:250,000 metallogenic map labels locality 255 the...]]></description><link>https://www.caadiametals.com.au/post/coopers-curraba</link><guid isPermaLink="false">6a619cd16ed1567a596f124d</guid><category><![CDATA[Mid-North-Coast]]></category><pubDate>Thu, 23 Jul 2026 04:50:28 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_bad06beead6b4e8781ee9dde99223bf6~mv2.png/v1/fit/w_705,h_539,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Mt Edith]]></title><description><![CDATA[Geological setting and mineral system Mt Edith is a low-sulphidation epithermal Au–Ag–Sb system in the Alum Mountain Volcanics at the northern closure of the Myall Syncline, southern New England Orogen — one of three documented epithermal prospects on a 25 km corridor classified in the open-file record as expressions of a single regional hydrothermal system (Nethery &#38; Jenkins 1988, R00005384). Diagnostic boiling-zone mineralogy — adularia + prehnite + bladed-carbonate pseudomorphs +...]]></description><link>https://www.caadiametals.com.au/post/mt-edith</link><guid isPermaLink="false">6a619b15424f5a9980a34db6</guid><category><![CDATA[Mid-North-Coast]]></category><pubDate>Thu, 23 Jul 2026 04:42:27 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_c4001a844b164104975a17edbc239014~mv2.png/v1/fit/w_630,h_547,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Cells Creek]]></title><description><![CDATA[Geological setting and mineral system The project sits in the Central Block of the New England Orogen and holds two gold occurrences ~1.6 km apart: the Cells Creek shear- and quartz-vein workings in Silurian metasediments, and the Oakbourne disseminated pyrite–gold prospect in altered high-K augite andesite whose albite–stilpnomelane–epidote assemblage Clutha reinterpreted as pre-metamorphic hydrothermal alteration (Temby 1994, R00001546). The combined signature — hydrothermal alteration,...]]></description><link>https://www.caadiametals.com.au/post/cells-creek</link><guid isPermaLink="false">6a619925424f5a9980a347c1</guid><category><![CDATA[Mid-North-Coast]]></category><pubDate>Thu, 23 Jul 2026 04:33:48 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_2c575689556a49239ec0a4564b0372f5~mv2.png/v1/fit/w_805,h_644,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Morton Deep]]></title><description><![CDATA[Geological setting and mineral system Hastings Block, eastern New England Orogen: granitoid-related Cu–Pb–Zn–Ag–Au–Sn–W mineralisation in Permian Beechwood Formation limestone–mudstone above the inferred Cairncross Adamellite heat source (government classification: "granitoid-related deposit", Gilligan &#38; Brownlow 1987, R00009339). The Median Anticline controls the architecture — the Greenbourne Creek Zone (GCZ) on the northern limb; the drilled Zone A (NP) and Zone B (HR/MC) clusters on the...]]></description><link>https://www.caadiametals.com.au/post/morton-deep</link><guid isPermaLink="false">6a619747424f5a9980a341df</guid><category><![CDATA[Mid-North-Coast]]></category><pubDate>Thu, 23 Jul 2026 04:27:06 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_a8550028e36945a298484972f0e8018a~mv2.png/v1/fit/w_897,h_610,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Basket Swamp]]></title><description><![CDATA[Geological setting and mineral system The prospect lies in the Permo-Triassic, high-K, I-type granite province of the Tenterfield–Stanthorpe region, southern New England Orogen, hosted entirely within the Lower Triassic Stanthorpe Adamellite (English 1996; GSNSW DIGS R00002143). Mineralisation occupies a steeply west-dipping structure striking 022°, expressed as a 15–20 m quartz–sericite alteration zone hosting a high-grade silver lode; old workings traceable ≈ 350 m north of the open cut...]]></description><link>https://www.caadiametals.com.au/post/basket-swamp</link><guid isPermaLink="false">6a617bfc6ed1567a596eb8ef</guid><category><![CDATA[Tenterfield]]></category><pubDate>Thu, 23 Jul 2026 02:30:21 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_6093bb8cefda40cc9c195077fe9f2bd7~mv2.png/v1/fit/w_707,h_340,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Plumbago Creek]]></title><description><![CDATA[Geological setting and mineral system Plumbago Creek sits in the Emu Creek Block of the southern New England Orogen, where the Permian Bruxner Park Adamellite (Pc_b, NSW Seamless Geology / MinView) intrudes a Carboniferous–Early Permian limestone–shale–chert sequence and marmorises the carbonate lenses. Government regional mapping classifies the iron bodies as probable contact skarns formed by reaction between the granite and the limey Permian sediments (Brownlow 1989, R00004511, p. 11)....]]></description><link>https://www.caadiametals.com.au/post/plumbago-creek</link><guid isPermaLink="false">6a6177e8f054ca40eb02eff6</guid><category><![CDATA[Tenterfield]]></category><pubDate>Thu, 23 Jul 2026 02:16:53 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_615c2ccab94c47fc977259eeb2a4f28b~mv2.png/v1/fit/w_737,h_556,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Back Creek]]></title><description><![CDATA[Geological setting and mineral system Back Creek is a five-occurrence prospect cluster (WN0006–WN0010) in hornfelsed Carboniferous Texas Beds on the western flank of the New England Orogen, ~30 km west of Tenterfield, NSW. GSNSW classifies all five occurrences as cassiterite (Sn) stockworks hosted in the Texas Beds (Brown, Henley &#38; Stroud 2001, GS2001/087); the As–Ag–Pb–Zn–Bi associations carried into targeting are the WMC 1992–95 rock-chip overlay (R00003116). CAADIA's working hypothesis...]]></description><link>https://www.caadiametals.com.au/post/back-creek</link><guid isPermaLink="false">6a616aee6ed1567a596e8a7e</guid><category><![CDATA[Tenterfield]]></category><pubDate>Thu, 23 Jul 2026 01:18:12 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_61e191a934584bf6ba9382a10da6e523~mv2.png/v1/fit/w_728,h_538,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Cowal]]></title><description><![CDATA[Geological setting and mineral system The ground lies within the Junee–Narromine Volcanic Belt of the Ordovician Macquarie Arc — a first-order copper–gold province hosting the Northparkes porphyry and, to the south-west, the Cowal gold deposit. The calcareous shelf sequence beneath the historical licence was recorded by the operator as prospective for replacement-style gold (R00004922, §2.2). The Wisdom Prospect carries an intrusion-related / distal-greisen signature (Au–As–Sb–W, low base...]]></description><link>https://www.caadiametals.com.au/post/cowal</link><guid isPermaLink="false">6a6169146ed1567a596e844f</guid><category><![CDATA[Macquarie Arc]]></category><pubDate>Thu, 23 Jul 2026 01:10:57 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_bd6fc510731a4ea0abf2ff1e97920825~mv2.png/v1/fit/w_852,h_585,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[West Forbes]]></title><description><![CDATA[Geological setting and mineral system West Forbes lies in the northern Junee–Narromine Volcanic Belt of the Ordovician Macquarie Arc — the principal host of porphyry and high-sulphidation epithermal Cu–Au mineralisation in NSW, whose type deposits (Northparkes, Lake Cowal) are concealed and were defined from drilling rather than outcrop (R00042286). Prospective arc basement is concealed here beneath an interpreted 100–140 m of Cainozoic and Mesozoic cover. The target model is a concealed,...]]></description><link>https://www.caadiametals.com.au/post/west-forbes</link><guid isPermaLink="false">6a6166ba6ed1567a596e7c72</guid><category><![CDATA[Macquarie Arc]]></category><pubDate>Thu, 23 Jul 2026 01:01:41 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_a6ff3bafc46c44f7adfbd11f5c518de6~mv2.png/v1/fit/w_799,h_515,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[Waratah]]></title><description><![CDATA[Geological setting and mineral system Concealed early-to-mid Palaeozoic basement interpreted as the north-western extension of the Junee–Narromine Volcanic Belt of the Macquarie Arc, straddling the Lachlan–Thomson orogen boundary, under 150–200 m of poorly lithified Mesozoic–Cainozoic cover; there is no Palaeozoic outcrop and no pre-existing stratigraphic drilling through the cover. The former holder's geophysical interpretation (Douglas Haynes Discovery, from GSNSW datasets including DIGS...]]></description><link>https://www.caadiametals.com.au/post/waratah</link><guid isPermaLink="false">6a611356424f5a9980a1bea2</guid><category><![CDATA[Macquarie Arc]]></category><pubDate>Wed, 22 Jul 2026 19:04:45 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_ec191feda2b342968c22ba50cd070401~mv2.png/v1/fit/w_832,h_515,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item><item><title><![CDATA[WOWINGRAGONG]]></title><description><![CDATA[Geological setting and mineral system The project sits in the concealed southern Junee–Narromine Volcanic Belt (JNVB) of the Macquarie Arc, Lachlan Orogen — the Ordovician–Early Silurian arc terrane whose principal endowments are intrusion-related, porphyry and porphyry-distal copper–gold systems, including Cowal, Northparkes and Marsden (Glen et al. 2007; analogues cited for geological context only). Basement beneath 3–37 m of alluvial cover at the historical collars (up to ~120 m...]]></description><link>https://www.caadiametals.com.au/post/wowingragong-project-summary</link><guid isPermaLink="false">6a60921688d0bba1346bfe0b</guid><category><![CDATA[Macquarie Arc]]></category><pubDate>Wed, 22 Jul 2026 09:53:30 GMT</pubDate><enclosure url="https://static.wixstatic.com/media/8e59ec_d768c645a6614411942edc7e9c4d5365~mv2.png/v1/fit/w_634,h_386,al_c,q_80/file.png" length="0" type="image/png"/><dc:creator>Doug Alcock</dc:creator></item></channel></rss>