Article
Geochemistry & Geophysics
Peter A. Cawood, Erin L. Martin, J. Brendan Murphy, Sergei A. Pisarevsky
Summary: After its assembly in the Ediacaran-Early Cambrian, Gondwana was surrounded by a system of peripheral orogens, including Terra Australis, Avalonian-Cadomian, and North Indo-Australie, which showed temporal correlations in their lithotectonic records. The development of these orogens was influenced by the breakup of Rodinia in the early Neoproterozoic, with variations reflecting the different relationships of their basement continental blocks to the supercontinent. The different orogens recorded the development of passive continental margins or convergent plate margins prior to Gondwana's assembly.
EARTH AND PLANETARY SCIENCE LETTERS
(2021)
Article
Geochemistry & Geophysics
F. A. Caxito, M. Heilbron, C. M. Valeriano, H. Bruno, A. Pedrosa-Soares, F. F. Alkmim, F. Chemale, L. A. Hartmann, E. Dantas, M. A. S. Basei
Summary: A robust dataset from Neoproterozoic igneous rocks in southeastern South America reveals a protracted consumption process of oceanic lithosphere, forming a Himalayas-sized orogenic belt. Time dependent isotopic variation trends suggest that Tonian-Cryogenian magmatic rocks formed in intra-oceanic supra-subduction settings.
GEOCHEMICAL PERSPECTIVES LETTERS
(2021)
Article
Geosciences, Multidisciplinary
Fabricio A. Caxito, Leo Afraneo Hartmann, Monica Heilbron, Antonio Carlos Pedrosa-Soares, Henrique Bruno, Miguel A. S. Basei, Farid Chemale
Summary: By analyzing data from various fields, it has been concluded that the South Atlantic Brasiliano Orogenic System went through a Wilson cycle involving different stages such as rift, drift, subduction, collision, and collapse. The evidence from petrographic, isotopic, and geophysical data reveals the complex evolution of the South Atlantic Brasiliano Orogenic System with distinct components of the Wilson cycle.
PRECAMBRIAN RESEARCH
(2022)
Article
Geosciences, Multidisciplinary
R. A. Glen, R. A. Cooper
Summary: New insights into the Late Precambrian-latest Devonian evolution of the Pacific margin of Gondwana reveal three key tectonic elements, suggesting that convergence along the margin was essentially simultaneous and showing possible trajectories of offshore terranes.
EARTH-SCIENCE REVIEWS
(2021)
Review
Geology
Biao Gao, Jitao Chen, Wenkun Qie, Xiangdong Wang
Summary: The Baoshan, Tengchong, Lhasa, South Qiangtang, and Sibumasu terranes were part of Gondwana before separating and moving away from the northern margin in the Early Permian. The paleopositions of these terranes during the late Paleozoic are still debated, which hampers the understanding of the tectonic evolution of the PaleoTethys and glacier distribution patterns on eastern Gondwana during the late Paleozoic ice age. Through analysis of detrital zircon U-Pb dating and Hf isotope signatures, this study proposes a new paleogeographic model that suggests the South Qiangtang, Baoshan, and part of Sibumasu were located outside the northern margin of Indian Gondwana, while the Lhasa and Sumatra terranes were along the northern margin of Australia. Based on shifts in provenance of late Paleozoic glaciogenic sedimentary rocks, the study also hypothesizes the development of two main ice sheets during the late Paleozoic. This research contributes to the understanding of the late Paleozoic tectonic and paleoclimatic history of Gondwana.
SEDIMENTARY GEOLOGY
(2022)
Article
Geosciences, Multidisciplinary
Johanna Van Daele, Dominique Jacques, Niels Hulsbosch, Stijn Dewaele, Philippe Muchez
Summary: The study focuses on the tectonic history of the Mesoproterozoic Karagwe-Ankole Belt in Central Africa's Western Domain, revealing two generations of folding believed to be the result of two separate compressional deformation events. The development of quartz veins provides chronological data, showing differences in tectonic history between the Western and Eastern Domain in the study area.
PRECAMBRIAN RESEARCH
(2021)
Article
Geosciences, Multidisciplinary
Zhensheng Li, Xueting Ma, Wei An, Ross N. Mitchell, Quanzhong Li, Zhongwu Lan, Yinxiao Dong, Yan Zhang, Jianxun Li
Summary: The study on the Bagongshan Group (BGG) of the Xuhuai Basin provides important constraints on the depositional age and provenance change of the North Qinling Terrane (NQT) in relation to the North China Craton (NCC). The results show that the accretion of NQT to NCC occurred before the deposition of the Liulaobei Formation at around 1.18 Ga, supporting the idea that NQT is a missing piece of the Grenvillian orogen in the reconstruction of the supercontinent Rodinia.
JOURNAL OF ASIAN EARTH SCIENCES
(2023)
Article
Geochemistry & Geophysics
Kabang'u G. Sakuwaha, Toshiaki Tsunogae, Patson Banda, Chela Changasha, Osbert N. Sikazwe, Yukiyasu Tsutsumi
Summary: The Zambezi Belt in southern Zambia and northern Zimbabwe is part of the Kuunga orogen, associated with the amalgamation of the Gondwana supercontinent. The belt consists of a basement and a supracrustal sequence, with different rock types. Petrographic and geothermobarometry analyses identified the presence of monazite in the crust, and revealed different tectonothermal histories. The rock units were brought together during the collision of the Congo and Kalahari Cratons.
Article
Geochemistry & Geophysics
Fengbo Sun, Peng Peng, Deshun Zheng, Pengfei Zuo
Summary: This study focuses on the early Neoproterozoic sediments in the southern-southeastern North China Craton (NCC) and their significance in paleogeographic reconstruction. New detrital zircon U-Pb-Hf data is presented for sandstone samples from the Sangwon Supergroup in SE-NCC and the Wufoshan Group in S-NCC, along with published zircon U-Pb data to determine their provenance. The results suggest a maximum depositional age of approximately 1.0 Ga for the Sangwon Supergroup and a possible extension of the Xuhuai-Dalian-Pyongnam basins in the SE NCC for the Wufoshan Group. The zircon age spectra show major populations at different time intervals, with potential contributions from the NCC and the southwestern Congo craton. The findings support a connection between the NCC and the southwestern Congo/SE NCC-S Sao Francisco at around 0.9 Ga. These results provide important insights into paleogeographic evolution.
Article
Geosciences, Multidisciplinary
Wei Wang, Peter A. Cawood, Manoj K. Pandit
Summary: The evolution of the Indian Block can be traced through Earth's supercontinent cycles, showing a close link with the events in the Cathaysia Block of South China. Terranes and microcontinents continued to accrete and collide along the western margin of the united North India-Cathaysia Block, leading to the formation of active continental margins and eventual collision with other blocks. The final assembly of Gondwana and Pangea involved the separation and drift of multiple continental blocks, eventually leading to the collision with the Asian segment of Pangea in the Permo-Triassic.
AMERICAN JOURNAL OF SCIENCE
(2021)
Article
Geosciences, Multidisciplinary
Wang Xu, Nigel C. Hughes, Lishuang Liu, Wen Zhang, Pinghua Liu
Summary: This study uses large sample zircon age data and mixing modeling method to investigate the paleogeographic position of the Lhasa terrane. The results suggest that during the Permo-Carboniferous, the Lhasa terrane received sediment from northwest Australia, aligning with stratigraphic and paleontological evidence from the northern margin of eastern Gondwana. The study highlights the effectiveness of the DZ mixing modeling method in constraining paleogeographic reconstruction.
GEOPHYSICAL RESEARCH LETTERS
(2022)
Article
Geosciences, Multidisciplinary
Ben Goscombe, David A. Foster, Dave Kelsey, Ben Wade, David Gray, Laura Mulrooney, Peng Jiang, Murray Haseler, Antonios Marsellos
Summary: Collision, high-angle contraction, crustal thickening and heating at 555-516 Ma primed the Damara Belt for crustal collapse. The collapse was triggered by a transition to ENE-WSW contraction along the belt in response to orogenic events in east Gondwana at 516-505 Ma. The high-grade core of the belt was reworked and thickened, leading to gravitational instability and the establishment of an extension direction across the belt. The collapse focused on the core, resulting in the formation of a metamorphic core complex with extensional shear zones and faults.
Article
Geosciences, Multidisciplinary
Lucia E. Gomez-Peral, M. Julia Arrouy, M. Sol Raigemborn, Camila Ferreyra, Victoria Penzo, Alcides N. Sial, Daniel G. Poire
Summary: The sedimentary infill of the Tandilia Basin underwent four different stages of deposition during the Neoproterozoic, two of which are visible in the Sierras Bayas Group and two in the La Providencia Group. The Villa Monica Formation represents the initial stage of basin infill and consists of a lower siliciclastic section transitioning into an upper dolostone section. The dolostone platform contains Cryogenian stromatolites and exhibits two distinct karst events.
INTERNATIONAL JOURNAL OF EARTH SCIENCES
(2023)
Article
Geosciences, Multidisciplinary
Jun-Yong Li, Xiao-Lei Wang, Di Wang, De-Hong Du, Jin-Hai Yu, Zhi-Dong Gu, Yu Huang, Lin-Sen Li
Summary: The Yangtze Block exemplifies the gradual formation of cratons since the Archean, and it is suggested to be divided into north and south parts due to distinct rock configuration and tectonic evolution. The block experienced Columbia assembly, supercontinent breakup, and accretion of terranes, involving extensional tectonics and seafloor spreading. These processes, along with mantle input and terrane accretion, contributed to the continental growth and reshaping of the Yangtze Block.
PRECAMBRIAN RESEARCH
(2021)
Article
Geosciences, Multidisciplinary
S. Aspiotis, S. Jung, F. Hauff, R. L. Romer
Summary: The study suggests that the Nomatsaus granite was formed in a continent-continent collisional setting with meta-igneous sources of possibly dacitic composition. Partial melting occurred during the initial stages of crustal heating, followed by mid-crustal level melting at higher P-T conditions and relatively late in the orogenic evolution. The petrogenetic model for the Nomatsaus granite is mainly based on the chemical characteristics and isotopic composition of the granite.
INTERNATIONAL JOURNAL OF EARTH SCIENCES
(2021)
Article
Geosciences, Multidisciplinary
Glenn R. Sharman, Theresa M. Schwartz, Lauren E. Shumaker, Cody R. Trigg, Nora M. Nieminski, Zachary T. Sickmann, Matthew A. Malkowski, Jeremy K. Hourigan, Benjamin J. Schulein, Stephan A. Graham
Article
Geology
Nora M. Nieminski, Stephan A. Graham
JOURNAL OF SEDIMENTARY RESEARCH
(2017)
Article
Geosciences, Multidisciplinary
Katherine L. Maier, Jennifer A. Gales, Charles K. Paull, Kurt Rosenberger, Peter J. Talling, Stephen M. Simmons, Roberto Gwiazda, Mary McGann, Matthieu J. B. Cartigny, Eve Lundsten, Krystle Anderson, Michael A. Clare, Jingping Xu, Daniel Parsons, James P. Barry, Monica Wolfson-Schwehr, Nora M. Nieminski, Esther J. Sumner
FRONTIERS IN EARTH SCIENCE
(2019)
Article
Geology
Katherine L. Maier, Charles K. Paull, David W. Caress, Krystle Anderson, Nora M. Nieminski, Eve Lundsten, Benjamin E. Erwin, Roberto Gwiazda, Andrea Fildani
JOURNAL OF SEDIMENTARY RESEARCH
(2020)
Article
Geosciences, Multidisciplinary
Jared T. Gooley, Nora M. Nieminski
Summary: This study investigates the sedimentary deposits of the East Coast Basin in New Zealand to unravel the evolution and sediment sources of Zealandia. The results indicate a transition in sediment source during the Early Cretaceous and major changes during the Late Cretaceous-Paleogene drift phase. Additionally, new volcanic activity and the formation of plate boundaries resulted in a new pattern of sediment routing.
Article
Geosciences, Multidisciplinary
M. Wolfson-Schwehr, C. K. Paull, D. W. Caress, R. Gwiazda, N. M. Nieminski, P. J. Talling, C. Carvajal, S. Simmons, G. Troni
Summary: This study demonstrates how ultra-high resolution seabed mapping using new technology can help understand the processes shaping submarine canyons. The study conducted time-lapse surveys of the Monterey Canyon axis, revealing centimeter-scale seabed textures and the effects of turbidity currents and internal tides. The results suggest that the scale gap between modern seafloor surveys and the ancient rock record may eventually be bridged with new mapping technology.
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
(2023)
Article
Environmental Sciences
Stephen C. C. Dobbs, Charles K. K. Paull, Eve M. M. Lundsten, Roberto Gwiazda, David W. W. Caress, Mary McGann, Marianne M. M. Coholich, Maureen A. L. Walton, Nora M. M. Nieminski, Tim McHargue, Stephan A. A. Graham
Summary: A high-resolution multibeam survey in the San Simeon Channel identified recurring troughs and ridges adjacent to meander bends. Through an integrated study, it was concluded that turbidity current event frequency was higher in the late Pleistocene due to sea-level rise and sediment sequestration on the shelf during the Holocene. This study highlights the significant decrease in sediment gravity flows in the region compared to times of continental shelf subaerial exposure.
FRONTIERS IN MARINE SCIENCE
(2023)