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searching for Petermann orogeny 16 found (19 total)

Petermann Orogeny (1,085 words) [view diff] case mismatch in snippet view article find links to article

The Petermann Orogeny was an Australian intracontinental event that affected basement rocks of the northern Musgrave Province and Ediacaran (Proterozoic)

Petermann Ranges (Australia) (278 words) [view diff] case mismatch in snippet view article

level. The range was formed about 550 million years ago during the Petermann Orogeny. The existing geological research has broadly determined that the

Musgrave Block (1,412 words) [view diff] case mismatch in snippet view article find links to article

The Musgrave Block is primarily exposed through the actions of the Petermann Orogeny at c. 535-550 Ma, which exhumed the orogenic belt along the Woodroffe

Lake Amadeus (543 words) [view diff] case mismatch in snippet view article find links to article

the Amadeus Basin that was filled with the erosion products of the Petermann Orogeny. Due to the aridity of the area, the surface of Lake Amadeus is usually

Centralian Superbasin (195 words) [view diff] case mismatch in snippet view article find links to article

disrupted by two periods of uplift and mountain building, Neoproterozoic Petermann Orogeny (by a central uplift and associated thrusts) and Palaeozoic Alice

Mann Ranges (269 words) [view diff] case mismatch in snippet view article find links to article

and Musgrave Ranges. Mountains in this region were formed in the Petermann Orogeny (600–550 million years ago). This area is part of the traditional

Alice Springs Orogeny (1,009 words) [view diff] case mismatch in snippet view article find links to article

north-south shortening: the late Neoproterozoic to early Cambrian Petermann Orogeny and the Devonian to Carboniferous Alice Springs Orogeny. The pattern

Amadeus Basin (361 words) [view diff] case mismatch in snippet view article find links to article

Centralian Superbasin. The basin was locally deformed during the Petermann Orogeny (late Neoproterozoic — Cambrian), and more extensively during the

Kata Tjuta (1,104 words) [view diff] case mismatch in snippet view article find links to article

during the Adelaidian, roughly 850–800 million years ago. During the Petermann Orogeny, approximately 550 million years ago, an event known as the Woodroffe

Geology of Australia (3,571 words) [view diff] case mismatch in snippet view article find links to article

Geosyncline (Adelaide Rift Complex) during the Neoproterozoic. The Petermann Orogeny caused extensive uplift, mountain building and basin fragmentation

Eclogite (1,812 words) [view diff] case mismatch in snippet view article find links to article

volcanics, mafic rocks and granulites occur in the Musgrave Block of the Petermann Orogeny, central Australia. Coesite- and glaucophane-bearing eclogites have

Eclogitization (1,467 words) [view diff] case mismatch in snippet view article find links to article

volcanics, mafic rocks and granulites occur in the Musgrave Block of the Petermann Orogeny, central Australia. Recently, coesite- and glaucophane-bearing eclogites

Hallett Cove Conservation Park (2,753 words) [view diff] case mismatch in snippet view article find links to article

2 Ma This mountain range may have been the southern extent of the Petermann Orogeny and part of a suspected Supermountain range that may have stretched

Geologic time scale (9,469 words) [view diff] case mismatch in snippet view article find links to article

continue to present day. First vertebrates from earlier chordates. Petermann Orogeny on the Australian continent tapers off (550–535 Ma). Ross Orogeny

Uluru (5,426 words) [view diff] case mismatch in snippet view article find links to article

were thrust up during a mountain building episode referred to as the Petermann Orogeny that took place in late Neoproterozoic to early Cambrian times (550–530

Timeline of natural history (7,668 words) [view diff] case mismatch in snippet view article find links to article

anemones. c. 550 Ma – Uluru or Ayers Rock begins forming during the Petermann Orogeny in Australia c. 544 Ma – The small shelly fauna first appears. c.