Home   |   About Journal   |   Editorial Board   |   Youth Editorial Board    |   Instruction   |   Ethics Statement   |   Open Access   |   Contacts Us   |   中文
  Office Online  
    Submission Online
    Peer Review
    Editor-in-chief
    Office Work
  Journal Online
    Accepted
    Current Issue
    Advanced Search
    Archive
    Read Articles
    Download Articles
    Email Alert
    
Quick Search  
  Adv Search
2014 Vol. 1, No. 2
Published: 2014-06-01
Orignal Article
 
       Orignal Article
1 Main Progress and Achievements in Regional Geological Survey of 1∶250 000 Changde Sheet
BAI Dao-yuan, MA Tie-qiu, WANG Xian-hui, CHEN Du-ping, PENG Yun-yi, ZHOU Ke-jun, LI Gang, HUANG Wen-yi
The regional geological survey project of 1∶250 000 Changde sheet have studied the Quaternary geological and environmental characteristics and evolution of the Dongting basin, and achieved progress as follows: ①We found out the Quaternary uplift-depression tectonic framework of the Dongting basin and peripheral area, and amply studied the Quaternary tectonic and sedimentary characteristics and environmental evolution of every secondary tectonic unit of the Dongting basin and its periphery area. ②We revealed the climatic evolution of the Dongting basin through pollen assemblages and geochemical characteristics of sediments, and discussed the evolutions of the sedimentary environment and tectonic subsidence of the southern Dongting basin through heavy minerals. ③We ascertained the tectonic movement characteristics of the basin that the Dongting basin was a rift basin during Early Pleistocene-middle of Middle Pleistocene, and entered into a depression phase since late Middle Pleistocene, and advanced geodynamic mechanism model of every tectonic period. ④We brought forward the concept of tectonic-sedimentary landforms, and defined tectonic-sedimentary landform types in the sheet.
2014 Vol. 1 (2): 1-6 [Abstract] ( 309 ) RICH HTML PDF (2077 KB)  ( 384 )
7 Main Progress and Achievements in Supplemental Regional Geological Survey of 1∶250 000 Yumenzhen Sheet
LIANG Ming-hong, HUO Qin-zhi, LI Hai-lin
The regional geological survey project of 1∶250 000 Yumenzhen sheet (K47C004001) has got some progress and achievements. In this project, we have found that the Dunhuang Group was mainly composed of a series of Paleoproterozoic khondalite rocks, and a set of epimetamorphic volcanic rocks, epimetamorphic fine clastic rocks and carbonate rocks. Combining with a large number of microfossil evidence, we confirmed that the three rock units were corresponding to the Qianluzigou group of Changcheng period, the Pingtoushan and Yema formation of Jixian, respectively. By using the innovative technology of finite strain measurement, five deformation events in the Dunhuang Group were identified on the basis of a detailed analysis of the ductile shear zone in this region. Through the statistics of the sedimentary grains, seven grain coarsening events in Changma alluvial fan were identified. Combining with a large number of ESR dating data, we suggested that the sediment grain size abrupt event and uplift of the plateau had a positive connection. In addition, we also found out the spatial-temporal distribution and evolution sequence of intrusive rocks in this region, and divided these intrusions into four types: homologous, heterologous, tectonic melange, and metamorphic.
2014 Vol. 1 (2): 7-14 [Abstract] ( 278 ) RICH HTML PDF (1736 KB)  ( 527 )
15 Main Progress and Achievements of Uranium Resource Investigation and Evaluation in Xuemisitan Volcanic Belt, Xinjiang
WANG Mou, LIU Jie
After summarizing the main progress and achievements of uranium resource investigation and evaluation, and after analyzing the regional metallogenic condition, we proposed that the Xuemisitan volcanic belt of Xinjiang province had favorable uranium metallogenic geological background. We summarized the characteristics of uranium mineralization in different regions according to the ore-controlling factors, such as the Baiyanghe uranium polymetallic deposit was controlled by the sub-volcanic contact zone, the Yinisala-Shiyuegongqu uranium ore concentration area was controlled by the secondary fissure zone, and the Mamente uranium ore occurrence was controlled by the collapsed volcanic apparatus. Combining with the geological conditions and the existing geological work, we forecasted the uranium prospecting areas, pointed out the future prospecting direction and proposed the following work suggestions
2014 Vol. 1 (2): 15-20 [Abstract] ( 308 ) RICH HTML PDF (1869 KB)  ( 277 )
21 Prospecting Progress and Indicators of the Tin Deposits in Xitian Metallogenic prospect area of Hunan Province—Prospective Survey Achievements of the Tin-Lead-Zinc Polymetallic deposit in Xitian, Hunan Province
WU Shi-chong, YU Yang-chun, ZENG Gui-hua, ZHU Hao-feng
The Xitian area is located at the northern margin of the east Hunan section in Nanling tungsten-tin-lead-zinc polymetallic metallogenic belt, and its geotectonic location is the junction belt between Yangtze Plate and Cathaysian Plate which has favorable metallogenic geological background. As an important territorial resources survey project approved by China Geological Survey in 2007, this project has deployed five aspects work as follows: 1∶50000 geological and mineral resources survey, ore area estimate, exploration demonstration, target verification, and comprehensive study. After a series of explorations and studies, we established the metallogenic geological model in Xitian area, brought forward the concept of "trinity ore-control system", determined the intrusive petrogenic age, determined the prospecting indicators, and figured out 301800 tons of tungsten and tin ore resources (332+333+334). However, as many mineral veins are still in pre-survey stage, we propose to increase exploration investment in further and to improve the resource level of Xitian area.
2014 Vol. 1 (2): 21-26 [Abstract] ( 345 ) RICH HTML PDF (1985 KB)  ( 288 )
27 Main Progress and Achievements of Strategic Mineral Prospective Survey Project of Nylonma Area, Tibet
YANG Chang-qing, LIU Wei, ZHAO Feng-yong, ZHAN Feng, GUO Jun-gong, WANG Liu-lin
In this project, the stratabound type and skarn type copper, lead, zinc, silver polymetallic deposit was selected as the main exploration target. We revealed the regional metallogenic geological background; found 111 mineralization anomalies; submitted 3 mineral deposits, 8 metallogenic areas and 23 prospecting target areas; established the prospecting indicators and prospecting model basing on a set of exploration methods includes 1:50000 geological mapping survey, ground magnetic survey, stream sediment survey, and remote sensing geological interpretation. In addition, we have the following new discoveries: 1) we recognized the Nyainqentanglha group complex, serpentinized peridotite and greisen-skarn type copper-tungsten deposit, skarn type bismuth deposits and indium deposit in the study area; 2) we found the Laigu formation and Mali formation have important exploration significance in Nyainqentanglha region, and proposed the regional sedimentary-transform metallogenic model. All these progress and achievements provide fruitful basic materials for further geological survey, mineral exploration and development.
2014 Vol. 1 (2): 27-34 [Abstract] ( 340 ) RICH HTML PDF (5082 KB)  ( 370 )
35 Main Progress and Achievements of the Permo-Carboniferous Petroleum Prospective Survey in Yine Basin and its Surrounding Areas
LU Jin-cai, CHEN Gao-chao, LI Yu-hong, WEI Xian-yang, ZHAO Xing-min, DANG Ben, CHEN Jian-fa, WEI Jian-she, JIANG Ting, LIU Jian-li, BO Jian-jun, YANG Gao-yin, SHI Ji-zhong, HAN Wei, LI Wei
As a production-study-research team, we solved the key problems affecting the petroleum geological conditions, and petroleum resources potential evaluation of the Permo-Carboniferous strata in Yingen-Ejina basin. Several new propositions about the formation and evolution mechanism of the basin, the distribution of sedimentary system and sedimentary facies, and source rocks have been established based on the theory of basin mountain coupling, as well as the geological and geophysical technology. The Yingen-Ejina and its surrounding area is a typical rift basin formed in Permo-Carboniferous period, and the source rocks are mainly deposited in the neritic shelf environment of Late Carboniferous and Early Permian. We found many sets of large thickness, stable lateral distribution, with little regional metamorphism, and mature-to-high-mature source rocks in the Permo-Carboniferous formation, accompanied by medium-to-high abundance marine organism and II type kerogen. Geochemical characteristics of natural gas and crude oil from the Upper Paleozoic weathered crust have significant relation with that of the Carboniferous source rocks. In addition, we forecasted the prospecting potential, favorable prospecting areas, and the relative benefit areas in the Permo-Carboniferous formation.
2014 Vol. 1 (2): 35-44 [Abstract] ( 328 ) RICH HTML PDF (3328 KB)  ( 303 )
45 Main Progress and Achievements of Land Subsidence Survey and Monitoring in Hebei Plain
ZHANG Jin-cai, CHU Li-feng, XIAO Zhen, LU Ze-chang, SHEN Rong-hui, CHEN Ying-jie
In this paper, the research background, research ideas, main work completed and research significance of “land subsidence survey and monitoring in Hebei Plain” are introduced, while the groundwater and ground fissure conditions of Hebei Plain, characteristics of the land subsidence monitoring network are summed up. The distribution rule, influencing factors, formation mechanism and harm characteristics of land subsidence are analyzed, and development trend of land subsidence in Cangzhou City, as the center of land subsidence in Hebei Plain, is forecasted also. In addition, reasonable countermeasures are put forward according to current situation of land subsidence.
2014 Vol. 1 (2): 45-50 [Abstract] ( 383 ) RICH HTML PDF (4770 KB)  ( 305 )
51 Main Progress and Achievements of Coastal Marine Geological Environment and Geological Hazard Investigation in Pearl River Delta
XIA Zhen, LIN Jin-qing, ZHENG Zhi-chang, SHI Yao-hong, MA Sheng-zhong, LIANG Kai, CHEN Tai-hao, HUANG Xiang-qing, ZHANG Shun-zhi, PAN Yi
A 1∶100000 coastal marine geological environment and geological hazard investigation was carried out for the first time in the Pearl River Delta, one of the most important economic zone in China, basing on integrated method of remote sensing, hydrology and hydrochemistry, comprehensive geophysical survey, geological sampling, geological drilling, and static sounding. The chemical parameter of seawater, marine environmental quality, hydrodynamics, topography and geomorphology, sediments, shallow stratigraphic structure, potential geological hazards and submarine engineering geological conditions were analyzed, and the marine geological environment was assessed and forecasted. Finally, reasonable suggestion about coastal marine development and engineering construction were put forward.
2014 Vol. 1 (2): 51-57 [Abstract] ( 392 ) RICH HTML PDF (1058 KB)  ( 378 )
58 Temporal and Spatial Evolution of the Granitoids from the Main Orogenic Belts in Asia and Their Implication for Tectonism and Metallogenesis
WANG Tao, TONG Ying, WU Cai-lai, WANG Xiao-xia, XIE Cai-fu, ZHANG Hong-rui, MAO Jian-ren, ZHANG Lei, HAN Bao-fu, GUO Lei, HONG Da-wei, WANG Yan-bin, ZHANG Jian-jun, LI Shan
Based on extensive collection of granitoid chronology data and information, a large number of fieldworks had been done in the key areas of the main orogenic belts in Asia, including foreign countries, such as Russia, Mongolia, Kyrgyzstan, South Korea, Japan, and Vietnam. Many high precision zircon U-Pb ages and geochemistry data had been got with a lot of careful analyses in laboratories, and some important magmatic events had been found. Combined with the high quality published data, the geochronological frameworks of granitoids from some key areas were built, and a preliminary summary of the temporal and spatial distribution and tectonic magmatic evolution of the granitoids from the Central Asian Orogenic Belt, Central Orogenic Belt (Qilian-Qinling). Tethys and West Pacific tectonic domain were obtained, providing relevant tectonic background for the mineral resources exploration. Based on above researches, a draft map of Asian granitoids with database has been made, and the tectonic evolution of Asian granitoids has also been published. It provides the basis for discussing the Asian tectonic evolution, especially for the process of continental convergence. This is the first approach to systematical discussion of the Asian granitoid magmatic evolution by Chinese researchers.
2014 Vol. 1 (2): 58-64 [Abstract] ( 441 ) RICH HTML PDF (2268 KB)  ( 757 )
  News
· 新一轮找矿突破战略行动专刊征稿启事
· 喜讯：中国地质图书馆（中国地质调查局地学文献中心）主办的《中国地质调查》连续第3年入选“中国科技核心期刊”
· 《中国地质调查》获得来自Scopus数据库的首个CiteScore
· 《中国地质调查》2024年第2期已在我刊网站发布
· 《中国地质调查》2024年第2期电子版已在中国知网发布
· 《中国地质调查》被美国化学文摘社（CAS）数据库收录
· 《中国地质调查》被中国科学评价研究中心评价为准核心学术期刊
· 地矿平台专业知识汇总，这一篇绝对够用！
  Download
2014—2023年《中国地质调查》期刊文献列表
《中国地质调查》论文模板
版权许可协议
  Links
22 Ministry of Natural Resources of the People's Republic of China
22 Geological Survey of China
22 National Geological Library of China
22 China Journal Full Database
22 Geological Society of China
22 Shandong Land and Resources
22 East China Geology
22 Chinese Library Classification
Copyright © Editorial Board of
Supported by: Beijing Magtech