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Mingcai Hou

Researcher at Chengdu University of Technology

Publications -  39
Citations -  408

Mingcai Hou is an academic researcher from Chengdu University of Technology. The author has contributed to research in topics: Zircon & Geology. The author has an hindex of 8, co-authored 39 publications receiving 174 citations.

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Geological and geochemical characteristics of marine-continental transitional shale from the Upper Permian Longtan formation, Northwestern Guizhou, China

TL;DR: In this article, the authors take the Upper Permian Longtan shale in the central Guizhou uplift as an example to characterize the transitional shale reservoir based on organic geochemistry data, X-ray diffraction (XRD) analysis, and scanning electron microscopy (SEM) observation.
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Characteristics and controlling factors of deep buried-hill reservoirs in the BZ19-6 structural belt, Bohai sea area

TL;DR: In this article, the BZ19-6 deep buried-hill structural belt in the southwest of Bozhong Sag, Bohai Bay Basin, is a newly discovered super-giant oil and gas bearing area, and the characteristics and control factors of reservoir development are not understood deeply.
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Provenance of latest Mesoproterozoic to early Neoproterozoic (meta)-sedimentary rocks and implications for paleographic reconstruction of the Yili Block

TL;DR: The Yili block is one of the major Precambrian microcontinents of the Central Asian Orogenic Belt (CAOB) as discussed by the authors, and Detrital zircon U-Pb ages and Hf isotopic data of the Meso-Neoproterozoic (meta)-sedimentary units within the Yili Block constrain the tectonic affinity and early history of the block.
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Intermediate-mafic dikes in the East Kunlun Orogen, Northern Tibetan Plateau: A window into paleo-arc magma feeding system

TL;DR: In this paper, the authors integrate data on the elemental and Sr-Nd-Hf isotope geochemistry, petrology, mineralogy, and zircon geochronology of late Permian dikes in the East Kunlun Orogen, northern Tibetan Plateau, discuss the petrogenesis of the dikes, and reconstruct the nature and relationship of different magma reservoirs.
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Neoproterozoic I-type and highly fractionated A-type granites in the Yili Block, Central Asian Orogenic Belt: Petrogenesis and tectonic implications

TL;DR: The Yili Block in NW China and NE Kazakhstan is a continental fragment within the Central Asian Orogenic Belt (CAOB) as discussed by the authors, and it has been identified as a Neoproterozoic granitic plutons from the southern Yili block to further constrain the evolution of microcontinents constituting the CAOB.