☆ 4.6 Review

Pre-Cryogenian stratigraphy, palaeontology, and paleogeography of the Tibetan Plateau and environs

SCIENCE CHINA-EARTH SCIENCES (2023)

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Diachronous subduction of the Proto-Tethys Ocean along the northern margin of East Gondwana: Insights from SHRIMP and LA-ICP-MS zircon geochronology in the West Kunlun Orogenic Belt, Northwestern China

Qinglin Sui et al.

Summary: This study provides information on the geological evolution of the Proto-Tethys Ocean by analyzing mineral geological data from the Tianshuihai Terrane. The results reveal that subduction-related magmatic activity in the Proto-Tethys Ocean occurred along the northern margin of the East Gondwana continent during the Late Neoproterozoic-Early Palaeozoic, gradually propagating to the east.

INTERNATIONAL GEOLOGY REVIEW (2023)

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Article Geosciences, Multidisciplinary

Paleogeographic Reconstruction of Precambrian Terranes Reworked by Phanerozoic Orogens: An Example Based on Detrital Zircon REE From Lhasa Terrane in Southern Tibet

Pei-yuan Hu et al.

Summary: Paleogeographic reconstruction of Precambrian terranes reworked by Phanerozoic orogens, such as the Tibetan Plateau, reveals complex lithotectonic relations due to intracrustal reworking. Global and regional detrital zircon rare earth element (REE) databases show trends in LREE/HREE and Eu/Eu* that record the crustal evolution of the source and provide a new approach for paleogeographic reconstructions. By analyzing sedimentary and igneous rocks in the Lhasa terrane and detrital zircon samples from the northern margin of Gondwana, it is demonstrated that the Lhasa terrane had an African affinity in the Rodinia-Gondwana supercontinent cycles (ca. 1.4-0.4 Ga).

GEOPHYSICAL RESEARCH LETTERS (2023)

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Article Geosciences, Multidisciplinary

A dynamic 2000-540 Ma Earth history: From cratonic amalgamation to the age of supercontinent cycle

Zheng-Xiang Li et al.

Summary: Understanding how tectonic plates have moved since deep time is crucial for comprehending the evolution and functioning of Earth's geodynamic system, as well as answering fundamental questions about plate tectonics. This knowledge has significant implications for various fields, including core-mantle-crust interaction, mountain building, and the formation of Earth resources, as well as global sea-level changes, climatic evolution, atmospheric oxygenation, and the evolution of life.

EARTH-SCIENCE REVIEWS (2023)

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Article Geosciences, Multidisciplinary

Progress towards an improved Precambrian seawater 87Sr/86Sr curve

Xi Chen et al.

Summary: The secular trend of seawater strontium isotope ratio provides important information about changes in ocean composition and global tectonic events. This study compiled and evaluated strontium isotope ratio data of Precambrian marine sedimentary rocks and generated an improved seawater Sr-87/Sr-86 curve. The results indicate an earlier deviation of seawater Sr-87/Sr-86 from the mantle, as well as stronger oscillations and better correspondence with supercontinent cycles than previously shown.

EARTH-SCIENCE REVIEWS (2022)

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Article Geology

South Tarim tied to north India on the periphery of Rodinia and Gondwana and implications for the evolution of two supercontinents

Peng Wang et al.

Summary: Constraining the positions of, and interrelationships between, Earth's major continental blocks has played a major role in validating the concept of the supercontinent cycle. The position of the Tarim craton is important for understanding the breakup of Rodinia and subsequent assembly of Gondwana. The ages and isotopic characteristics of detrital zircons in the South Tarim and north India support the idea that Tarim was located on the margin of both supercontinents. The tectonic transitions and drift between North Tarim and South Tarim emphasize the importance of retreating subduction in supercontinent dispersal.

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Middle Neoproterozoic (ca. 700 Ma) tectonothermal events in the Lhasa terrane, Tibet: Implications for paleogeography

Pei-yuan Hu et al.

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Precambrian metamorphic basement of the southern Lhasa terrane, Tibet

Xin Dong et al.

Summary: The study on orthogneisses in the Milin area of the southeastern Lhasa terrane provides insights into the local protolith crystalline ages and their relation to the Neoproterozoic-Paleozoic strata in the Lhasa terrane. Geochemical data suggests the Mesoproterozoic rocks may have originated from partial melting of Paleoproterozoic crustal materials, representing the Precambrian metamorphic basement of the Lhasa terrane.

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Neoproterozoic and Early Paleozoic magmatism in the eastern Lhasa terrane: Implications for Andean-type orogeny along the northern margin of Rodinia and Gondwana

Yanfei Chen et al.

Summary: The magmatic activities in the Lhasa terrane during the Precambrian and Early Paleozoic are crucial for understanding the geological history of the North and South Lhasa terranes as well as the northern margins of the Rodinia and Gondwana supercontinents. A study of the Bomi complex in the Lhasa terrane revealed Neoproterozoic and Cambrian magmatic events, with evidence of crustal melting and mantle-derived magmas. These findings suggest the presence of distinct Precambrian basements in the North and South Lhasa terranes.

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Secular Evolution of Continents and the Earth System

Peter A. Cawood et al.

Summary: Understanding the secular evolution of the Earth system is essential for studying the history of our planet. By analyzing the rock and mineral archive in the continental lithosphere, researchers have identified seven phases of secular evolution. Integrating this record with knowledge of mantle cooling and lithospheric rheology provides insights into the changes in tectonic modes throughout Earth's history.

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A newly discovered Neoproterozoic diamictite-cap carbonate couplet from the Western Himalaya: The expansion of the Marinoan snowball Earth glaciation to the northwestern margin of the Indian Plate in North Pakistan

Malik Muhammad Saud Sajid Khan et al.

Summary: This study provides convincing evidence of the glacial diamictite-cap carbonate couplet from the Tanakki Member in the Western Himalaya, helping to overcome previous glacio-stratigraphic discrepancies and revise the stratigraphic framework in the region.

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Spatial distribution of 1.4-1.3 Ga LIPs and carbonatite-related REE deposits: Evidence for large-scale continental rifting in the Columbia (Nuna) supercontinent

Shuan-Hong Zhang et al.

Summary: A large-scale continental rift zone dating back to 1.4-1.3 billion years ago has been identified along western Laurentia, western-northern Siberia, southeastern Baltica, western-northern West Africa, southwestern Amazonia, southern-eastern Congo/Sao Francisco, eastern Kalahari, northern North China, and northern North Australia. This rift zone, extending approximately 15,000 km across the supercontinent Columbia, played a significant role in its breakup. The spatial distribution of REE deposits associated with carbonatite intrusions further supports the importance of this rift system in controlling the formation of major rare earth element deposits.

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Widespread magmatic provinces at the onset of the Sturtian snowball Earth

Kai Lu et al.

Summary: Research finds that the Franklin large igneous province (LIP) existed about 717 million years ago, just before the onset of the Sturtian snowball Earth, indicating widespread magmatic activity in various regions prior to the glaciation. It suggests that low-to-mid-latitude volcanism in the millions of years preceding the Sturtian enhanced global weatherability, creating a cool background climate for the stratospheric sulfate aerosol injection caused by the Franklin eruption.

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Lin Ding et al.

Summary: This review discusses the temporal and spatial distribution of surface uplift in the Tibetan Plateau and the geodynamic mechanisms behind it. The initial collision between India and Asia and the subsequent formation of the high Tibetan Plateau are still not well understood, but the uplift is primarily controlled by delamination and break-off of the subducted Indian and Asian lithosphere.

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Early Neoproterozoic granitic gneisses in the Amdo micro-continent, Tibet: petrogenesis and geodynamic implications

Yun-Peng Yu et al.

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Neoproterozoic Amdo and Jiayuqiao microblocks in the Tibetan Plateau: Implications for Rodinia reconstruction

Yiming Liu et al.

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GEOLOGICAL SOCIETY OF AMERICA BULLETIN (2021)

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Paleomagnetic constraints on the duration of the Australia-Laurentia connection in the core of the Nuna supercontinent

Uwe Kirscher et al.

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The role of megacontinents in the supercontinent cycle

Chong Wang et al.

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GEOLOGY (2021)

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A Neoproterozoic low-δ18O magmatic ring around South China: Implications for configuration and breakup of Rodinia supercontinent

Hao Zou et al.

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Were South India, the North China Craton, and the Korean Peninsula contiguous in a Neoarchaean supercontinent? New geochemical and isotopic constraints

P. V. Thanooja et al.

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LITHOS (2021)

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Neoproterozoic bimodal magmatism in the eastern Himalayan orogen: Tectonic implications for the Rodinia supercontinent evolution

Zhi Zhang et al.

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SCIENCE (2021)

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Gondwana's interlinked peripheral orogens

Peter A. Cawood et al.

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EARTH AND PLANETARY SCIENCE LETTERS (2021)

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Qing Wang et al.

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GEOPHYSICAL RESEARCH LETTERS (2021)

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Zhengfu Guo et al.

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Xin Dong et al.

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Yue Tang et al.

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Pei-yuan Hu et al.

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Wei Wang et al.

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The Apparent Polar Wander Path of the Tarim block (NW China) since the Neoproterozoic and its implications for a long-term Tarim-Australia connection

P. Zhao et al.

PRECAMBRIAN RESEARCH (2014)

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A rapid and synchronous initiation of the wide spread Cryogenian glaciations

Zhongwu Lan et al.

PRECAMBRIAN RESEARCH (2014)

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Re-Os geochronology and coupled Os-Sr isotope constraints on the Sturtian snowball Earth

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PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA (2014)

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Not all supercontinents are created equal: Gondwana-Rodinia case study

Christopher J. Spencer et al.

GEOLOGY (2013)

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The origin and pre-Cenozoic evolution of the Tibetan Plateau

Di-Cheng Zhu et al.

GONDWANA RESEARCH (2013)

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Paleomagnetism of the late Cryogenian Nantuo Formation and paleogeographic implications for the South China Block

Shihong Zhang et al.

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Isotopic ages for alkaline igneous rocks, including a 26 Ma ignimbrite, from the Peshawar plain of northern Pakistan and their tectonic implications

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Gondwana dispersion and Asian accretion: Tectonic and palaeogeographic evolution of eastern Tethys

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JOURNAL OF ASIAN EARTH SCIENCES (2013)

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The Carboniferous ophiolite in the middle of the Qiangtang terrane, Northern Tibet: SHRIMP U-Pb dating, geochemical and Sr-Nd-Hf isotopic characteristics

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Precambrian evolution of the Lhasa terrane, Tibet: Constraint from the zircon U-Pb geochronology of the gneisses

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Tectonic evolution of the Eastern Ghats Belt, India

Somnath Dasgupta et al.

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U-Pb zircon age and Hf isotope compositions of Mesoproterozoic sedimentary strata on the western margin of the Yangtze massif

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SCIENCE CHINA-EARTH SCIENCES (2013)

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Archean Subduction: Fact or Fiction?

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ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 40 (2012)

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U-Pb geochronology of basement rocks in central Tibet and paleogeographic implications

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Early Paleoproterozoic rift volcanism in the eastern Fennoscandian Shield related to the breakup of the Kenorland supercontinent

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The making of Gondwana: Discovery of 650 Ma HP granulites from the North Lhasa, Tibet

Zeming Zhang et al.

PRECAMBRIAN RESEARCH (2012)

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Precambrian geology of China

Guochun Zhao et al.

PRECAMBRIAN RESEARCH (2012)

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A Change in the Geodynamics of Continental Growth 3 Billion Years Ago

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Discovery of ∼4.0 Ga detrital zircons in the Changdu Block, North Qiangtang, Tibetan Plateau

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Lhasa terrane in southern Tibet came from Australia

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Assembly and breakup of the core of Paleoproterozoic-Mesoproterozoic supercontinent Nuna

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Triassic eclogites from central Qiangtang, northern Tibet, China: Petrology, geochronology and metamorphic P-T path

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Recognition of Grenvillian volcanic suite in the Shennongjia region and its tectonic significance for the South China Craton

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The discovery of Palaeoproterozoic volcanic rocks in the Bulunkuoler Group from the Tianshuihai Massif in Xinjiang of Northwest China and its geological significance

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Detrital zircon geochronology of pre-Tertiary strata in the Tibetan-Himalayan orogen

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The mountains that triggered the Late Neoproterozoic increase in oxygen: The Second Great Oxidation Event

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Geologic correlation of the Himalayan orogen and Indian craton: Part 2. Structural geology, geochronology, and tectonic evolution of the Eastern Himalaya

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Calibrating the Cryogenian

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Neoproterozoic hydrothermally altered basaltic rocks from Rajasthan, northwest India: Implications for late Precambrian tectonic evolution of the Aravalli Craton

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Eocene melting of subducting continental crust and early uplifting of central Tibet: Evidence from central-western Qiangtang high-K calc-alkaline andesites, dacites and rhyolites

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The Grenvillian and Pan-African orogens: World's largest orogenies through geologic time, and their implications on the origin of superplume

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Geological and geochronological evidence for the Precambrian evolution of the Tarim Craton and surrounding continental fragments

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Assembling Australia: Proterozoic building of a continent

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Assembly, configuration, and break-up history of Rodinia: A synthesis

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Paleoproterozoic granitic gneisses of the Dinggye and LhagoiKangri areas from the higher and northern Himalaya, Tibet: Geochronology and implications

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Geochronologic constraints on the chronostratigraphic framework of the neoproterozoic Huqf Supergroup, Sultanate of Oman

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Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry

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The huqf supergroup of Oman: Basin development and context for neoproterozoic glaciation

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Geochemistry and tectonic significance of basaltic lavas in the Neoproterozoic Yanhian Group, Southern Sichuan Province, Southwest China

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Linking accretionary orogenesis with supercontinent assembly

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EARTH-SCIENCE REVIEWS (2007)

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Early palaeozoic orogenesis along the Indian margin of Gondwana: Tectonic response to Gondwana assembly

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4.1 Ga old detrital zircon in western Tibet of China

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CHINESE SCIENCE BULLETIN (2007)

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Late Mesoproterozoic to earliest Neoproterozoic basin record of the Sibao orogenesis in western South China and relationship to the assembly of Rodinia

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Correlation of lithotectonic units across the eastern Himalaya, Bhutan

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The Yanbian terrane (Southern Sichuan Province, SW China): A neoproterozoic are assemblage in the western margin of the Yangtze block

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Integrated tectonostratigraphic analysis of the Himalaya and implications tor its tectonic reconstruction

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Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent

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EARTH-SCIENCE REVIEWS (2002)

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SHRIMP U-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze Block, South China

MF Zhou et al.

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Early Neoproterozoic magmatism (1000-910 Ma) of the Zadinian and Mayumbian Groups (Bas-Congo):: onset of Rodinia rifting at the western edge of the Congo craton

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U-Pb zircon ages from the Indian plate in northwest Pakistan and their significance to Himalayan and pre-Himalayan geologic history

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Geochemical evolution of peraluminous paleoproterozoic bandal orthogneiss NW, Himalaya, Himachal Pradesh, India: implications for the ancient crustal growth in the Himalaya

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Suturing of the Proto- and Paleo-Tethys oceans in the western Kunlun (Xinjiang, China)

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Geochronological constraints for a two-stage history of the Albany-Fraser Orogen, Western Australia

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Radiating 1.0 Ga mafic dyke swarms of eastern Brazil and western Africa: Evidence of post-assembly extension in the rodinia supercontinent?

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Tectonic implications of U-PL zircon ages of the Himalayan orogenic belt in Nepal

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