中国地质灾害类型图_葛中远编,_地貭矿产部成都水文地貭工程地貭中心编_,_主编,_葛中远

China is an emerging superpower, with a huge demand for raw materials and mineral resources that are being used to increase the standard of living conditions for its residents and bolster its surge forward in the global economy. To enable this rapid growth, China is also undertaking an education revolution with the help of experts from around the world in many different fields of endeavour.

Modern Fluvial-Deltaic Deposits in Daihai Lake Basin, Northern China
Shunli Li, Chengpeng Tan, Xin Shan, Xinghe Yu, and Xuefa Shi

Core Investigation of the International Continental Scientific Drilling Program from the Cretaceous Songliao Basin (SK-1/SK-2/ SK-3), NE China
Yuan Gao, Youfeng Gao, and Daniel E.

Ibarra Cambrian Tempestites in the Xiaweidian Area, Western Beijing City
Bo Liu, Kaibo Shi, Hangyu Liu, Chun Wu, and Qing He

Lower Cretaceous Lacustrine Sedimentary Sequences of a Small Intracontinental Rift Basin in Luanping, China
Ping Luo, Chuanmin Zhou, Xingyang Zhang, Zhijie Zhang, Xuanjie Zhang, and Xiufen Zhai Songliao

Molybdenum (Mo) is a transition metal with an atomic number of 42 and a relative atomic mass of 95.95. Important isotopes are 95Mo, 96Mo, and 98Mo. Molybdenum has a high melting point of 2623
C and one of the lowest coefficients of thermal expansion among commercially used metals. It readily forms hard, stable carbides in alloys and is widely used in steel alloys, including high-strength alloys and superalloys. Molybdenum was discovered in 1781 by Peter Jacob Hjelm and the name is from the Greek “molybdos,” which means “lead,” because it was often confused

with lead. Details on the chemistry and uses of molybdenum can be found at www. rsc.org/periodic-table/element/42/molybdenum.

As a country rich in mineral resources, contemporary China remains surprisingly overlooked in the research about the much debated ‘resourcecurse’. This is the first full-length study to  examine the distinctive effects of mineral resources on the state, capital and labour and their interrelations in China. Jing Vivian Zhan draws on a wealth of empirical evidence, both qualitative and quantitative. Taking a subnational approach, she zooms in on local situations and demonstrates how mineral resources affect local governance and economic as well as human development.

In 1916, the first generation of geological graduates entered the China Geological Survey and opened a new era of geological survey in China. Over the past 100 years, generations of geologists have made outstanding contributions to the geological survey and prospecting for China’s prosperity. They measure the ground, search for treasures, explore the earth, and engrave the beautiful mountains and rivers.

In 2014, China has continued the implementation of National Exploration and Development Planning and achieved outstanding progress in geological prospecting, and it is the reserves & resources of major mineral resources that increased obviously. There is a sustainable growth in the production and import of major mineral products as well as a further improvement in the supplying capacity. Efforts have been made to promote the survey and evaluation of geology and mineral resources, and better social services. To facilitate the construction of ecological civilization, China has paid more attention to enhance the environmental recovery of mines, and over 25% of the land damaged by mining development has been reclaimed.

Тектонический контроль, реконструкция и консервация тигелонгнанского месторождения порфиров и эпитермальных отложений меди (Au), Центральный Тибет, Китай

The newly discovered Tiegelongnan Cu (Au) deposit is a giant porphyry deposit overprinted by a high-sulfidation epithermal deposit in the western part of the Bangong–Nujiang metallogenic belt, Duolong district, central Tibet. It is mainly controlled by the tectonic movement of the Bangong–Nujiang Oceanic Plate (post-subduction extension). After the closure of the Bangong–Nujiang Ocean, porphyry intrusions emplaced at around 121 Ma in the Tiegelongnan area, which might be the result of continental crust thickening and the collision of Qiangtang and Lhasa terranes, based on the crustal radiogenic isotopic signature.