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Devonian integrative stratigraphy, biotas, and paleogeographical evolution of the Qinghai-Tibetan Plateau and its surrounding areas
The Devonian System in the Qinghai-Tibetan Plateau and its surrounding areas is widely distributed, diverse in lithotypes and rich in fossils. It...
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Contrasts between the Interannual Variations of Extreme Rainfall over Western and Eastern Sichuan in Mid-summer
Rainfall amount in mid-summer (July and August) is much greater over eastern than western Sichuan, which are characterized by basin and plateau,...
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Anisotropy of magnetic susceptibility of the Late Cretaceous–Eocene sediments in the southeastern Fenwei Graben and its tectono-sedimentary significance
The Fenwei Graben located in the conjoint region between the Neo-Tethys tectonic domain and the western Pacific tectonic domain is key to...
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Using Spatial Autocorrelation for the Hypsometric Integral to Differentiate Geology and Neotectonics: A Case Study in Bailongjiang Drainage Basin (Eastern Tibet Plateau)
Hypsometric integral (HI) has been widely used in Geomorphology study as an index to depict the recent and active structures for its sensitivity to...
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Differences and variations in the elevation-dependent climatic growing season of the northern and southern slopes of the Qinling Mountains of China from 1985 to 2015
Based on daily mean temperature data from 32 meteorological stations in the study area, this paper discusses the relationship between the changes in...
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Extreme large-scale atmospheric circulation associated with the “21·7” Henan flood
From July 19 to 21, 2021, Henan, a province in northern China (NC), was affected by severe flooding (referred to hereafter as “21·7”) caused by a...
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Analysis of Magnetic Field Distribution and Magnetic Susceptibility of the Lithosphere in East Dabie Region, China: Relationship to Crustal Structures
AbstractIn order to study in detail the characteristics of the lithospheric magnetic field and underground magnetic susceptibility structure in the...
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Basin Uranium Mineralization Law
Research on the distribution of uranium deposits and anomalies in drilling data indicate that sandstone-type uranium mineralization in the Ordos...
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Origin of Chromitites in the Songshugou Peridotite Massif, Qinling Orogen (Central China): Mineralogical and Geochemical Evidence
The Songshugou peridotite massif is located in the north of Shangdan suture zone, North Qinling orogenic belt of Central China. The massif is mainly...
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Transformation and mechanisms of climate wet/dry change on the northern Tibetan Plateau under global warming: A perspective from paleoclimatology
The northern Tibetan Plateau is a climatically sensitive zone influenced by monsoon and westerly winds. In summer, water vapor transport can reach...
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Heterogeneous metal sources for mintage in the early Han empire, second century BCE: archaeometallurgical study of the Banliang coins from the Guanghuacun cemetery, Chengdu, Southwest China
The supply of metal materials for mintage is important for state governance, and the patterns of which appear to reflect the rise and decline of the...
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Geoheritage Geomorphology of an Alpine Region in Northwest China: Introduction to the Yeliguan National Geopark
The Yeliguan region is located in Northwest China and consists of outcrops from Carboniferous to Quaternary age. This region, affected by the uplift...
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Introduction
This chapter focuses on the concept and classification of tunnel boring machine (TBM), its origin, development, and application in the world,...
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Zircon Hf Isotope Map** for Understanding Crustal Architecture and Its Controls on Mineralization during Early Cretaceous in the Southern Great **ng’an Range, NE China
Voluminous Early Cretaceous granitoids and associated large-scale ore deposits are distributed within the southern Great **ng’ an Range (SGXR), NE...
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Precipitation scale effect of the TRMM satellite in Tianshan, China
High-resolution precipitation data is conducive to objectively describe the spatial-temporal variability of regional precipitation, and the study of...
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Background of the Ordos Basin
The Ordos Basin is located in the central part of North China, with its main body located in Shanxi Province, Inner Mongolia Autonomous Region.
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Pre-Cryogenian integrative stratigraphy, biotas, and paleogeographical evolution of the Qinghai-Tibetan Plateau and its surrounding areas
The composition and geological evolution of pre-Cryogenian material in the Tibetan Plateau and its surrounding areas have played an important role in...
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Analysis of ecological drought risk characteristics and leading factors in the Yellow River Basin
With the increasing number and intensity of drought events, understanding the ecological drought risk in the Yellow River Basin has become an...
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Experimental study on the failure mechanism of the Zhoujiashan landslide under the combined effect of rainfall and earthquake in Tianshui City, Northwest China
Catastrophic loess-mudstone landslides have long been a major concern in Northwest China due to the extreme weather and frequent earthquakes in...
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Changes in characteristics of climate extremes from 1961 to 2017 in Qilian Mountain area, northwestern China
In this study, the temporal and spatial characteristics of extreme climate from 1961 to 2017 were analyzed using daily precipitation and temperature...
