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Mingzhu Ma

Publications -  27
Citations -  1944

Mingzhu Ma is an academic researcher. The author has contributed to research in topics: Zircon & Craton. The author has an hindex of 21, co-authored 24 publications receiving 1555 citations.

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Zircon ages and geochemistry of late Neoarchean syenogranites in the North China Craton: A review

TL;DR: In this paper, two phases of syenogranite magmatism are recognized based on geological relationships, degree of metamorphism, deformation and magmatic zircon ages.
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Episodic Paleoproterozoic (~2.45, ~1.95 and ~1.85 Ga) mafic magmatism and associated high temperature metamorphism in the Daqingshan area, North China Craton: SHRIMP zircon U-Pb dating and whole-rock geochemistry

TL;DR: In the Daqingshan area within the Khondalite Belt of the North China Craton, Paleoproterozoic gabbro and dolerite intrusions show amphibolite to granulite-facies metamorphism as mentioned in this paper.
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Juvenile magmatism and crustal recycling at the end of the Neoarchean in Western Shandong Province, North China Craton: Evidence from SHRIMP zircon dating

TL;DR: Wang et al. as mentioned in this paper used SHRIMP zircon dating of thirty-one samples of different rock types from late Neo-archean rocks yielded a narrow age range from 2560 to 2490 Ma.
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Multiple 3.8–3.1 Ga tectono-magmatic events in a newly discovered area of ancient rocks (the Shengousi Complex), Anshan, North China Craton

TL;DR: In this paper, the authors report the full geological context for more ancient rocks from a third Anshan locality, the polyphase migmatite Shengousi Complex, and show that the geology of this area has a strong similarity with the Narryer Gneiss Complex of Western Australia, which contains polyphase Eoarchaean Meeberrie gneisses, the 3490-3440-Ma Eurada gniss association, ∼3300-Ma granites and migmatisation, and is intercalated with younger Precamb
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Early Neoarchean (∼2.7 Ga) tectono-thermal events in the North China Craton: A synthesis

TL;DR: The North China Craton (NCC) is characterized by major ∼2.5 Ga tectono-thermal events and is thus different from many other cratons worldwide where ∼ 2.7 Ga events are well developed as mentioned in this paper.