A geophysically constrained crustal element map of East Antarctica between Enderby Land and Princess Elizabeth Land

IF 1.2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Y. Giri, P. Betts, M. Radhakrishna, M. McLean, T. K. Biswal, R. Armit
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引用次数: 1

Abstract

Abstract East Antarctica along with Greater India played a vital role in the accretion and breakup of the Indo-Antarctic landmasses during the supercontinents Nuna, Rodinia and Gondwana. Without geophysical potential field methods, interpreting the architecture of the ice-covered geological provinces of Antarctica is impossible. We present here a crustal element map of East Antarctica between Enderby Land and Princess Elizabeth Land (Indo-Antarctica tectonic element) using aerogeophysical data interpretation. The data reveal distinct anastomosing geophysical provinces that correlate with sparse geological data. Our crustal element map shows the Oygarden Province and the Northern and Southern Rayner provinces are arcuate belts that wrap around the Archean Napier Province. These provinces represent the remnants of an accretionary tectonic margin, which evolved between ca 1300 Ma and 900 Ma. The arcuate geometry of these Meso- to Neoproterozoic provinces formed during the collision with the Napier Province, which represents a microcontinent. This collision triggered widespread extension and ultra-high temperature metamorphism in the Northern and Southern Rayner provinces. The southernmost provinces include the Fisher Province, Lambert Province and a transition zone. The provinces are truncated by a suture zone with the Archean Ruker Province, following north-dipping subduction during the Meso- to Neoproterozoic. Our interpretation provides a template upon which to correlate geological provinces with the terranes on the conjugate eastern Indian margin. KEY POINTS An aeromagnetic interpretation is given for Enderby Land and Princess Elizabeth Land of East Antarctica. Napier Province is a microcontinent that collided with the Rayner Province during a ca 1000 Ma orogenic event. A new interpretation of potential field data suggests anastomosing provinces accreted as part of a collisional event. New structures/piercing points are identified at the Mawson Coast and in Kemp Land.
南极洲东部恩德比地和伊丽莎白公主地之间的地球物理约束地壳元素图
在努纳、罗迪尼亚和冈瓦纳超大陆时期,东南极洲和大印度在印度-南极大陆块的增生和分裂中起了至关重要的作用。如果没有地球物理势场方法,就不可能解释南极洲被冰覆盖的地质省份的结构。本文利用航空地球物理资料解释,绘制了Enderby Land和Princess Elizabeth Land(印-南极洲构造元素)之间的东南极洲地壳元素图。这些数据揭示了与稀疏的地质数据相关的独特的吻合的地球物理省。我们的地壳元素图显示,Oygarden省和Rayner省的北部和南部是环绕太古宙Napier省的弧形带。这些省份代表了一个增生构造边缘的残余,在大约1300 Ma和900 Ma之间演化。这些中至新元古代省的弧形几何形状是在与纳皮尔省碰撞时形成的,代表了一个微大陆。这次碰撞在雷纳省北部和南部引发了广泛的伸展和超高温变质作用。最南端的省份包括费舍尔省、兰伯特省和一个过渡区。中-新元古代北倾俯冲,与太古宙鲁克省形成缝合带。我们的解释提供了一个模板,在此基础上将地质省与共轭东印度边缘的地体联系起来。给出了东南极洲恩德比岛和伊丽莎白公主岛的航磁解译。纳皮尔省是一个微大陆,在大约1000 Ma的造山活动中与雷纳省碰撞。对势场数据的一种新的解释表明,重合的省份是碰撞事件的一部分。在莫森海岸和坎普地发现了新的构造/刺穿点。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Australian Journal of Earth Sciences
Australian Journal of Earth Sciences 地学-地球科学综合
CiteScore
2.80
自引率
8.30%
发文量
45
审稿时长
6-12 weeks
期刊介绍: Australian Journal of Earth Sciences publishes peer-reviewed research papers as well as significant review articles of general interest to geoscientists. The Journal covers the whole field of earth science including basin studies, regional geophysical studies and metallogeny. There is usually a thematic issue each year featuring a selection of papers on a particular area of earth science. Shorter papers are encouraged and are given priority in publication. Critical discussion of recently published papers is also encouraged.
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