Mainstage mineralisation is spatially related to the roof and border zones of several high level, post-kinematic, geochemically specialized, Permian granites. The following types of mineralisation phenomena are recognised and described1) pervasive. postmagmatic metasomatisms and alterations 2) hydrothermal breccia pipes 3) metallised and non-metallised pegmatites 4) metallised vein systems 5) metallised replacements. These mineralisation phenomena show definite space-time patterns within the batholith and its environs. Five spatial environments are recognised each, characterised by a particular style of mineralisation at any point in time. Mainstage mineralisation is considered to have been emplaced in four distinct phases, which broadly co...
The United North Australian Mine lies within a roof pendant of sedimentary rocks of Silurian- Devoni...
Mineralization is localized in a series of emanative centers which trend parallel with, and lie adja...
Examination of the microstructural and textural development of the lead-zinc mineralisation at Mount...
This study addresses the hydrothermal alteration and mineralization related to a system of tourmalin...
International audienceThe Achmmach tin mineralization (NE of theMoroccan Central Massif) is associat...
The timing and kinematics of regional deformation play a key role in granite pluton construction, as...
The metalliferous ore deposits of southwest England are associated with biotite-muscovite granites t...
In the Kinta Hills area marble, quartzite, schist and argillite have been intruded by coarse-grained...
A porphyry-stock-related style of mineralisation in the Grampian Terrane is characterised by a stock...
The mineralization in Perlombongan Maju Hin Lee, is essentially hydrothermal in origin. The primary ...
The North Pennine Orefield Alston Block has produced approximately 4 Mt Pb, 0.3 Mt Zn, 2.1 Mt fluori...
This item is only available electronically.The Moonta-Wallaroo area has been of economic, historical...
The E31 copper-gold prospect is one of several porphyry or porphyry related prospects that occur ad...
The Pb - Zn - Ba - F deposits of the Southern Pennine Orefield comprise stratabound rakes, pipes, an...
Tasmania is the most important tin province in Australia, having been endowed with >0.65 Mt Sn. Some...
The United North Australian Mine lies within a roof pendant of sedimentary rocks of Silurian- Devoni...
Mineralization is localized in a series of emanative centers which trend parallel with, and lie adja...
Examination of the microstructural and textural development of the lead-zinc mineralisation at Mount...
This study addresses the hydrothermal alteration and mineralization related to a system of tourmalin...
International audienceThe Achmmach tin mineralization (NE of theMoroccan Central Massif) is associat...
The timing and kinematics of regional deformation play a key role in granite pluton construction, as...
The metalliferous ore deposits of southwest England are associated with biotite-muscovite granites t...
In the Kinta Hills area marble, quartzite, schist and argillite have been intruded by coarse-grained...
A porphyry-stock-related style of mineralisation in the Grampian Terrane is characterised by a stock...
The mineralization in Perlombongan Maju Hin Lee, is essentially hydrothermal in origin. The primary ...
The North Pennine Orefield Alston Block has produced approximately 4 Mt Pb, 0.3 Mt Zn, 2.1 Mt fluori...
This item is only available electronically.The Moonta-Wallaroo area has been of economic, historical...
The E31 copper-gold prospect is one of several porphyry or porphyry related prospects that occur ad...
The Pb - Zn - Ba - F deposits of the Southern Pennine Orefield comprise stratabound rakes, pipes, an...
Tasmania is the most important tin province in Australia, having been endowed with >0.65 Mt Sn. Some...
The United North Australian Mine lies within a roof pendant of sedimentary rocks of Silurian- Devoni...
Mineralization is localized in a series of emanative centers which trend parallel with, and lie adja...
Examination of the microstructural and textural development of the lead-zinc mineralisation at Mount...