Understanding the Bushveld Igneous Complex: A Large 2 Billion-Year-Old Intrusion in South Africa
Bushveld is a large igneous intrusion that occurs in the Transvaal region of South Africa. It covers an area of approximately 65,000 square kilometers and is estimated to be around 2 billion years old. The Bushveld Complex is one of the largest layered intrusions in the world and is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Complex is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Complex is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Complex is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Complex is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Complex is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Complex is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Complex is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Complex is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Complex is a large igneous province that covers an area of approximately 65,000 square kilometers in the Transvaal region of South Africa. It is estimated to be around 2 billion years old and is one of the largest layered intrusions in the world. The BIC is composed of a variety of rocks including granite, pegmatites, and quartz-feldspar porphyries.
The Bushveld Igneous Complex (BIC) is a large igneous province that covers an area of approximately
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