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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Far East
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China
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Hainan China (1)
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Kunlun Mountains (2)
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Yunnan China
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Tengchong (2)
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Taiwan
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Tatun Shan (1)
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Tibetan Plateau (1)
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United States
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New York
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Livingston County New York (1)
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Wyoming County New York (1)
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geochronology methods
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Ar/Ar (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene (3)
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Pleistocene
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upper Pleistocene (1)
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igneous rocks
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igneous rocks
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volcanic rocks
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basalts
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shoshonite (1)
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volcanic ash (1)
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Primary terms
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absolute age (1)
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Asia
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Far East
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China
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Hainan China (1)
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Kunlun Mountains (2)
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Yunnan China
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Tengchong (2)
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Taiwan
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Tatun Shan (1)
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Tibetan Plateau (1)
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Cenozoic
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Quaternary
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Holocene (3)
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Pleistocene
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upper Pleistocene (1)
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data processing (2)
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deformation (1)
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fractures (1)
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igneous rocks
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volcanic rocks
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basalts
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shoshonite (1)
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pyroclastics (1)
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lava (1)
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magmas (1)
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mantle (1)
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New York
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Two discrete gold mineralization events recorded by hydrothermal xenotime and monazite, Xiaoqinling gold district, central China
Perspectives on the active volcanoes of China
Abstract China has a rich record of Holocene volcanism that is relatively little known outside the country. It is encountered in large stratovolcanoes in the NE, linked to subduction of the Pacific plate (e.g. Changbaishan), in smaller volcanoes on the Tibetan margin, associated with the collision of India and Eurasia (e.g. Tengchong, Ashishan), and in more isolated centres, possibly resulting from mantle upwelling (e.g. volcanoes in Hainan island). This makes China a natural laboratory for studies of intraplate volcanism, and significant progress in understanding its nature and origins has been made over the past quarter century. Here, we introduce the first publication in English to provide a comprehensive survey of the state of knowledge and research highlights. Accordingly, we provide an overview of the dynamics, geology, geochemistry, volcanic histories and geophysical studies of 14 volcanic areas associated with the Holocene documented thus far. The special publication represents a benchmark reference on the topic but, as importantly, we hope that it will stimulate new, international collaborations aimed at deepening our understanding of the origins, history, hazards and associated risks of China's volcanoes.
Volcanic geology and petrochemistry of Ashikule volcanic field in western Kunlun Mountains of the Tibetan plateau
Abstract Ashikule volcanic field, developed in the western Kunlun mountain of north Tibet, is composed of approximately 10 volcanoes, and covers a total area of about 200 km 2 at an average altitude of approximately 5000 m, one of the highest volcanic fields in the world. In this study, we conducted detailed field investigations of the geological and geomorphological features of volcanic rocks and volcanic edifices in Ashikule basin, and compiled a large-scale geological map of the study area for the first time. We also collected a series of samples for petrochemistry analysis, as well as a high-precision 40 Ar/ 39 Ar geochronology study of selected lavas from Ashikule volcanic field. Finally, we refined the eruption history for the volcanic activity in the basin, which provides some new volcanological evidence for the study of the tectonic evolution of the Northern Tibetan Plateau.
Abstract In the West Kunlun Mountains, four volcanic fields (Kangxiwa, Dahongliutan, Qitaidaban and Quanshuigou) are distributed along the Dahongliutan fault, which is c. 180 km long. Based on field investigations, chronological measurements and geochemical analysis of some volcanic fields, the results of geological, geochemical and geophysical research in previous studies in the corresponding study areas are summarized. The volcanic activities in these areas were mainly effusive eruptions, explosive eruptions and phreatomagmatic eruptions. In this study, we discovered the Qitaiyanhu volcanic field for the first time and determined that the 14 C age of the lacustrine strata underlying the Qitaiyanhu lava flows is 13.110 ± 0.04 ka BP, indicating that there may still have been volcanic activities in the late Pleistocene and even the Holocene in the Dahongliutan fault area. Base surge deposits, which are the products of the interaction between magma and water, were found in the Kangxiwa volcanic field. The four shoshonitic rock fields of Kangxiwa, Dahongliutan, Qitaidaban and Quanshuigou are likely to be products of different evolution stages from the same magma source area. The magmatic origin of these volcanic fields may be related to the upwelling of the asthenosphere, triggered by the collision between the Indian and Tarim plates.
Abstract China has numerous active volcanoes, and more than 10 erupted in the Quaternary. Although a modern eruption event has not occurred in China, the potential risk from volcanic hazards should be noted. With the development of geodetic technologies including the Global Positioning System (GPS), levelling and interferometric synthetic aperture radar (InSAR), volcanologists can now detect the present-day deformation state of China's active volcanoes. In this paper, we summarize the present-day deformation patterns, magma sources and magma plumbing systems of China's active volcanoes between 1970 and 2013. The results show that the most active volcano in China is the Changbaishan volcano; it showed significant inflation from 2002–03, with the deformation becoming gradually weaker after 2003, indicating that it had been experiencing a magma process during 2000–10. A point source at a depth of c. 10 km was responsible for the observed deformation. The Leiqiong volcanic field showed a trough pattern deformation during 2007–10, which was interpreted as a dyke intrusion model. Fluctuant deformation patterns were shown in the Tengchong volcanic field. The Longgang volcanic field had experienced a volcano-wide uplift during the 1970s and 1990s. Deformation was observed in the Tatun volcanic field from 2006–13, and two shallow sources account for the observed deformation. These volcanoes merit further monitoring given possible evidence of deformation. No obvious deformation related to volcanic activity was observed at the Ashikule volcanic field from 2003–11. The results provide a basic introduction to the deformation state of China's active volcanoes, and may be helpful for evaluating the activity levels of China's volcanoes and mitigating the risks of future volcanic hazards.
The impact of volcanic ash on the safety of aviation industry: review of China's current situation
Abstract By synthesizing relevant research findings from China and other countries, this paper discusses the distribution and eruption types of volcanoes in China. An analysis of the spreading characteristics of volcanic ash possibly caused by volcanic eruptions such as those from Changbaishan is presented, and the impact of volcanic ash on aviation flight safety, as well as several key methods of monitoring volcanic ash, are discussed. This paper also outlines the operational process of China's aviation industry in addressing volcanic ash and compares and analyses the handling of volcanic ash by civil aviation industries globally. Further, ways of dealing with volcanic ash are then suggested for China's aviation industry.
Knowledge base of Cenozoic volcanoes in China
Abstract Knowledge management plays an important role in scientific research and provides a basis for technical development in the era of Big Data. Studies of Cenozoic volcanoes in China have been undertaken for more than half a century, generating plentiful relevant literature and data. However, these data have stayed scattered between different authors and libraries, and this hampers management and access. Based on theories, knowledge bases and related technologies, we developed the Knowledge Base of Cenozoic Volcanoes (KBCV) to collect such volcanic data in China. The directory tree of the KBCV is structured based on five levels according to the volcano distribution, magma origin, data type and file format. The KBCV supports querying, searching and browsing. It can provide well-managed Cenozoic volcanic data and technical support for scientific research and public communication. The KBCV is still in its early stages and is imperfect with respect to data completeness and universalization of the system, and efforts are being made to continuously develop and popularize the system.
Methodology for remote characterization of fracture systems in bedrock of enemy underground facilities
Abstract Weaponry can be conveniently and safely concealed in enemy underground bedrock facilities (UGF). The bedrock environment surrounding UGF offers a high degree of protection for the assets contained within. Physical characteristics of the surrounding bedrock constrain the effects of conventional and even nuclear weapons. Brittle structures in the bedrock such as fracture systems have anisotropic characteristics and present a formidable obstacle to the survival of penetrating weapons. Knowledge of the three-dimensional (3-D) characteristics of bedrock fracture systems in enemy UGF, which may be covered by soil or vegetation, is of paramount importance to the weapons development community in its quest to penetrate anisotropic environments. We utilize rigorous methodologies to predict fracture characteristics in overburden-covered regions from outcrop, core, borehole, and remote sensing data. We have established digital scanline and scangrid methodologies to characterize fracture geometries. The digital data allow us to easily analyze the fractures in terms of fractal and more advanced geostatistical techniques. We have developed theoretical and practical guidelines for determining the two-dimentional (2-D) density of fractures from one-dimentional (1-D) (scanline) data. Additionally, we have developed theoretical relationships between 2-D and 3-D fracture densities. Integration of digital field data with density and spatial structure of the fracture networks allows us to predict the distribution of fractures in areas removed from the outcrop. These methodologies, once refined, fully tested, and verified, will allow us to characterize three-dimensional fracture systems in potential target areas worldwide by remote sensing means alone.