Polyphase Deformation of the High-Grade Metamorphic Rocks along the Neusspruit Shear Zone in the Kakamas Domain: Insights into the Processes during the Namaquan Orogeny at the Eastern Margin of the Namaqua Metamorphic Province, South Africa
Abstract
:1. Introduction
2. Geological Setting
3. Methodology
4. Results
4.1. Lithostratigraphy
4.1.1. Supracrustal Rocks
Puntsit Formation
Goede Hoop Formation
4.1.2. Plutonic Rocks
Basement
Kakamas Suid Gneiss
Riemvasmaak Gneiss
Warm Zand Leucogneiss
Friersdale Charnockite
4.2. Metamorphism
4.3. Structure
4.3.1. Neusberg Macrofold
4.3.2. Structural Fabrics and Related Metamorphic Grade
Sub-Area 1
Sub-Area 2
Sub-Area 3
4.4. Thrusting
4.5. Shearing
4.5.1. Shear Sense Indicators
4.5.2. Kinematic Analysis
5. Discussion
5.1. Basement/Cover Stratigraphy
5.2. Comparison of Sub-Areas
5.3. Metamorphism and Deformation
5.3.1. M1 and D1 Events
5.3.2. M2 and D2 Events
5.3.3. M3 and D3 Events
5.3.4. M4 and D4 Events
5.4. Tectonic Evolution
6. Conclusions
Supplementary Materials
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Group | Subgroup | Suite | Formation/Nature | Member/Unit | Rock Type | Age (Ma) | Thickness (m) | Description |
---|---|---|---|---|---|---|---|---|
Keimoes | Friersdale Charnockite | Intrusive rock | 1113–1080 | Opalescent blue quartz, lenses of felsic and mafic composition, medium- to coarse-grained, granoblastic texture | ||||
Non-conformity | ||||||||
Korannaland | Goede Hoop (Fluviatile) | Feldspathic mica-rich quartzite | Supracrustal rock | 140–200 | Medium to coarse-grained quartzite, granoblastic texture, well-bedded, presence of pebbles, extensively intruded by Friersdale Charnockite, biotite gneiss within the contact zone | |||
Biesie Poort | Puntsit (psammitic and calcareous with intercalations of likely basaltic material) | Calc-silicate-rich quartzite with intercalations of amphibole schist | 30–80 | Fine- to medium-grained quartzite, granoblastic texture, presence of intercalations of fine-grained amphibole schist, well-bedded, lenses of skarn and wollastonite-bearing calcareous rock | ||||
Non-conformity | ||||||||
Warm Zand leucogneiss | Intrusive rock | Brown in colour, fine- to medium-grained, quartz and feldspar, faint streaks of amphibole and biotite, granoblastic texture | ||||||
Riemvasmaak Gneiss | Pink in colour, medium- to coarse-grained, quartz and feldspar, amphibole and biotite, granoblastic texture | |||||||
Kakamas Suid Gneiss | Grey to brown in colour, augen texture, feldspar mylonites, inequigranular showing augen texture |
Deformation Event | Age (Ma) | Magmatism | Metamorphism | Structure | Characteristic | Fabric | Deformation Style |
---|---|---|---|---|---|---|---|
D1a | ~1200 | a T = ~800 °C P = 5.5 kbar | Inter-terrane thrust (HBRT) | Compressional deformation | start of progressive shear | ||
D1b | F₁ folding | D₁bF₁ folds, transposition S₀ into S₁ | S₁ shear fabric | progressive shear continuing | |||
D2 | ~1155–1110 | Syn-tectonic plutons | b T = 700–660 °C P = 5.5 kbar | F₂ folding | D₁bF1 folds, S2 axial planar, S₁/S₂ co-planar | S₂ regional fabric | Main progressive shear |
D3 | c 1113 to 1080 | Post-tectonic Friersdale Charnockite of the Keimoes Suite | d T = ~640–550 °C P = 4.8 kbar | Friersdale Charnockite into D₁b fold hinge | Weakly defined fabric | Progressive shear terminated | |
D4 | e T = ~350 °C P = ~3.5 kbar | Reactivation of intra-terrane thrust, formation of transcurrent shear zone | Northwest-trending steeply inclined shear zone, shear direction towards east | Deformation of adjacent pre-existing structure | Start of transpressional shearing |
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Tsakou Sonwa, C.S.; van Bever Donker, J.; Bailie, R. Polyphase Deformation of the High-Grade Metamorphic Rocks along the Neusspruit Shear Zone in the Kakamas Domain: Insights into the Processes during the Namaquan Orogeny at the Eastern Margin of the Namaqua Metamorphic Province, South Africa. Minerals 2021, 11, 759. https://doi.org/10.3390/min11070759
Tsakou Sonwa CS, van Bever Donker J, Bailie R. Polyphase Deformation of the High-Grade Metamorphic Rocks along the Neusspruit Shear Zone in the Kakamas Domain: Insights into the Processes during the Namaquan Orogeny at the Eastern Margin of the Namaqua Metamorphic Province, South Africa. Minerals. 2021; 11(7):759. https://doi.org/10.3390/min11070759
Chicago/Turabian StyleTsakou Sonwa, Cyrille Stephane, Jan van Bever Donker, and Russell Bailie. 2021. "Polyphase Deformation of the High-Grade Metamorphic Rocks along the Neusspruit Shear Zone in the Kakamas Domain: Insights into the Processes during the Namaquan Orogeny at the Eastern Margin of the Namaqua Metamorphic Province, South Africa" Minerals 11, no. 7: 759. https://doi.org/10.3390/min11070759