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341
A carbon isotope reference curve for ca. 1700-1575 Ma, McArthur and Mount Isa Basins, northern Australia
Published 2000“…The results of this study, combined with earlier studies on younger rocks, imply that the global ocean reached a state of equilibrium in the mid-Paleoproterozoic and remained stable for much of the following billion years. …”
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342
Trans-Hudson Orogen of North America and Himalaya-Karakoram-Tibetan Orogen of Asia: Structural and thermal characteristics of the lower and upper plates
Published 2006“…The Trans-Hudson Orogen (THO) of North America and the Himalaya-Karakoram- Tibetan Orogen (HKTO) of Asia preserve a Paleoproterozoic and Cenozoic record, respectively, of continent-continent collision that is notably similar in scale, duration and character. …”
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343
Exotic accessory minerals in layered chromities of the Campo Formoso complex (Brazil)
Published 2006-01-01“…The Campo Formoso stratiform intrusive complex, in Bahia State, Brazil, considered to be of Paleoproterozoic age, consists of a tabular body of ultramafic rocks about 40 km long and 100-1100 m wide. …”
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344
Melt-melt immiscibility and implications for the origin of Madeira albite-rich granite, Pitinga mine, Amazonas, Brazil: A melt inclusion study
Published 2022-01-01“…Abstract Presented here are the results of the first studies of silicate melt inclusions hosted in quartz crystals from the two late granitic facies of the Paleoproterozoic Madeira pluton in the Pitinga mine, State of Amazonas, Brazil. …”
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345
Reaction-diffusion modelling of petrological mixing mechanisms in the evolution of continental crusts
Published 2023-12-01“…This study examines the mechanisms of such macroscopic assimilation between felsic (F) and mafic (M) constituents as two petrologically interacting continuum phases, as observed in the Chotanagpur Granite Gneissic Complex (CGGC), India, which underwent amphibolite to granulite facies metamorphism (∼775 to 900°C and 7 to 11 kb) between from the Paleoproterozoic to the late Mesoproterozoic. From field investigation we could recognized four interface patterns: planar, wavy, fingering and incoherent, which are generated at the interface between the F and M units. …”
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346
A Novel Workflow for Geothermal Prospectively Mapping Weights-of-Evidence in Liaoning Province, Northeast China
Published 2017-07-01“…Geological faults are highly developed in the eastern Liaoning Province in China, where Mesozoic granitic intrusions and Archean and Paleoproterozoic metamorphic rocks are widely distributed. …”
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347
DIBROVSKOE URANIUM-TORIUM-RARE-EARTH ORE OCCURRENCE OF THE UKRAINIAN SHIELD (LITHO-STRATIGRAPHIC CRITERIА OF THE GENESIS AND LOCALIZATION OF ORE BODIES)
Published 2019-08-01“…These deposits and ore manifestations are localized in the formation rocks of ancient metamorphosed con-glomerates, gravelites and sandstones and belong to a single stratigraphic level – the base of the paleoproterozoic protoplatform cover. New mineralogical and geochemical data have been obtained confirming the initially sedimentary (alluvial) genesis of thorium-rare-earth concentrations of the Dibrovskoe ore occurrence. …”
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348
Chemolithotrophy in the continental deep subsurface: Sanford Underground Research Facility (SURF), USA
Published 2014-11-01“…SURF provides access into an iron-rich Paleoproterozoic metasedimentary deposit that contains deeply circulating groundwater. …”
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349
Poly-Orogenic Melting of Metasedimentary Crust From a Granite Geochemistry and Inherited Zircon Perspective (Southern Calabria-Peloritani Orogen, Italy)
Published 2019-05-01“…Abundant inherited zircon cores from representative samples of metamorphosed late Cadomian (545 ± 5 Ma) granite and late Variscan (300 ± 4 Ma) leucogranodiorite have the same range of U–Pb ages, from Early Paleoproterozoic to latest Neoproterozoic, with main age clusters at ∼0.55 and ∼0.63 Ga, and minor age clusters at ∼0.95 and ∼2.5 Ga. …”
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350
Litsa uranium ore occurrence (Arctic zone of the Fennoscandian Shield): new results of petrophysical and geochemical studies
Published 2022-07-01“…According to homogenization temperatures of inclusions in liquid phase, the temperature of the Paleoproterozoic and Paleozoic stages of uranium mineralization at the Litsa ore occurrence is ~ 300 and 200 °С, respectively. …”
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351
Stratigraphic sequence characteristics and geochronology research progress of the Cenozoic in the arcuate tectonic belt on the northeastern margin of the Tibet Plateau
Published 2023-08-01“…This paper systematically studied the Paleoproterozoic to Neoproterozoic sedimentary sequences and stratigraphic ages in the arcuate tectonic belt. …”
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352
Multidisciplinary Modeling of Mantle Lithosphere Structure Within the Superior Craton, North America
Published 2021-04-01“…Prominent east‐ and west‐dipping mantle structures relate best to a Paleoproterozoic (Trans‐Hudson) deformation, which is rarely observed in the crust. …”
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353
Evaluating the Compatibility of Hematite (U‐Th)/He Data and Hematite‐Carried Secondary Magnetizations: An Example From the Colorado Front Range
Published 2023-09-01“…Here, we compare hematite He data and paleomagnetic results in Paleoproterozoic crystalline rocks, meters below a major nonconformity in the Colorado Front Range, USA. …”
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354
Evolution of metamorphic processes in the Neoarchean mafic granulites of the Qingyuan Terrane in northern Liaoning, North China Craton
Published 2023-10-01“…The second-generation metamorphic assemblage is characterized by locally formed coronas or symplectites of garnet + quartz ± clinopyroxene, representing high-pressure (HP) granulite facies metamorphism associated with a Paleoproterozoic orogenic event.…”
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355
Komatiites From Mantle Transition Zone Plumes
Published 2020-09-01“…The distinctive geodynamic setting of Gorgona Island produced relatively low-temperature komatiites at the only place along the margin of North and South America where it was possible to reproduce the bowl-like subduction configurations commonly associated with their Archean and Paleoproterozoic counter parts.…”
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356
Composition and P-T conditions of the lithospheric mantle beneath the Azimuth 125º Lineament, Northern and Southern Brazil: constraints from peridotite xenoliths enclosed in diamon...
Published 2022-10-01“…The data indicate that the cratonic 40 mW/m2 geothermal gradient in Rondônia may be related to a process of thermal relaxation of the lithospheric mantle after the Paleoproterozoic to Mesoproterozoic tectonothermal events of the southwestern Amazonian Craton until the sampling of the xenoliths by the magma in the Permian-Triassic. …”
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357
Garnet granulites of Sutam River middle current sutam river (Aldan Shield) as possible indicators of metamorhosed and tectonically displaced Post-Hadean weathering crust
Published 2017-12-01“…The diapirism of garnet granulites (with the captured Hadean zircon) proceeded during the Paleoproterozoic thermotectogenesis of the Aldan shield which were accompanied by the horizontal propagation of deep-seated granite-anorthosite tectonic flows from the plume’s center to its periphery. …”
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358
Cambrian/Ordovician boundary as a milestone in the sedimentation history of the southern Siberian craton: Evidence from U-Pb dating of detrital zircons
Published 2022-12-01“…The U-Pb ages of detrital zircons from the sampled Upper Lena Fm. sandstones are mostly Early Paleozoic (∼500 Ma), with very few Archean-Paleoproterozoic determinations and quite many Neoproterozoic zircons. …”
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359
MINERAL POTENTIAL OF ARCTIC KARELIA
Published 2018-02-01“…Aunique complexly folded structure ofpolymetamorphic rocks, which evolved in polychronous manner, was formed. The Early Paleoproterozoic rift-induced system, tens of kilemetres in width, extending along the boundary between the Karelian and the Belomorian provinces, has a common source of mantle magma formation. …”
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360
Constraints on the lithospheric structure and tectonics of Archean Dharwar Craton, southern India from geophysical and geological data: Evidence for modified lithosphere
Published 2022-11-01“…It has experienced several tectonic and magmatic events, including mafic dykes of various periods since Paleoproterozoic. The Dharwar Craton was accreted with the Karwar and Coorg blocks on the west and Eastern Ghats and Nallamalai fold belts on the east during the Proterozoic. …”
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