1:50 000 Mineral Geological Map Database of the Huaniushan Map-sheet, Gansu

WANG Chunnv; DU Zezhong; YU Xiaofei; LI Yongsheng; LV Xin; SUN Hairui; DU Yilun

doi:10.12029/gc2019Z107

2019 Vol. 46, No. S1

Article Contents

Article navigation > Geology in China > 2019 > 46(S1): 55-65

Next Article Previous Article

WANG Chunnv, DU Zezhong, YU Xiaofei, LI Yongsheng, LV Xin, SUN Hairui, DU Yilun. 2019. 1:50 000 Mineral Geological Map Database of the Huaniushan Map-sheet, Gansu[J]. Geology in China, 46(S1): 55-65. doi: 10.12029/gc2019Z107

Citation:

WANG Chunnv, DU Zezhong, YU Xiaofei, LI Yongsheng, LV Xin, SUN Hairui, DU Yilun. 2019. 1:50 000 Mineral Geological Map Database of the Huaniushan Map-sheet, Gansu[J]. Geology in China, 46(S1): 55-65. doi: 10.12029/gc2019Z107

1:50 000 Mineral Geological Map Database of the Huaniushan Map-sheet, Gansu

1.
Development and Research Center of China Geological Survey, Beijing 100037, China
2.
Mineral Exploration Technical Guidance Center, Ministry of Natural Resources, Beijing 100120, China

Fund Project: China Geological Survey Project "Demonstration of Prospecting Prediction and Technical Application in Integrated Survey Areas" (121201004000172201).

More Information

Author Bio: WANG Chunnv, female, born in 1986, engineer and master engages in mineral prediction; E-mail: wangchunnv009@163.com
Corresponding author: DU Zezhong, male, born in 1986, senior engineer and docter engages in research into typical deposits and prospecting prediction; E-mail:27793009@qq.com

Received Date: 06 March 2019

Revised Date: 31 May 2019

Publish Date: 25 June 2019

Abstract

Abstract

The 1:50 000 mineral geological map of the Huaniushan map-sheet (K46E017023), Gansu province, is developed in accordance with the Technical Specification for Mineral Geological Survey (1:50 000) and unified standards and requirements in the sector, building on making full use of results from and information of 1:200 000 and 1:50 000, etc. regional geological survey, applying the digital mapping system to plot geology-specific maps in the field and adopting the method integrating indoor and outdoor mapping and compilation. In this map, the formation type of the Nanhua-system-Sinian-system Xichangjing Group, Cambrian-system Xishuangyinshan Formation and Ordovician-system Huaniushan Group is reclassified, the periods of intrusive rocks in the map sheet are included in three periods, i.e. late Ordovician epoch-early Silurian epoch, Devonian period and late Triassic epoch, and the evolutionary sequence of magmatite. The database contains data and information of 12 stratigraphic units and magmatite of three periods, with a data size about 3.77 MB. These data fully reflect demonstrative results from the 1:50 000 mineral geological survey, provide a reference to mineral resource research and energy exploration in the area.
- Mineral geological mapping /
- Huaniushan map-sheet /
- 1:50 000 /
- Database /
- Gansu

FullText(HTML)

References

[1]	Kröner A, Hegner E, Lehmann B, Heinhorstc J, Wingated MTD, Liue DY, Ermelovf P. 2008. Palaeozoic arc magmatism in the Central Asian Orogenic Belt of Kazakhstan: SHRIMP zircon ages and whole-rock Nd isotopic systematic[J]. Journal of Asian Earth Sciences, 32(2): 118−130. Google Scholar
[2]	Xiao WJ , Mao QG , Windley BF , Han CM, Qu JF, Zhang JE, Ao SJ, Guo QQ, Cleven NR, Lin SF, Shan YH, Li LJ. 2010. Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage[J]. American Journal of Science, 310(10): 1553−1594. doi: 10.2475/10.2010.12 CrossRef Google Scholar
[3]	苗来成, 朱明帅, 张福勤. 2014. 北山地区中生代岩浆活动与成矿构造背景分析[J]. 中国地质, 41(4): 1191−1204. Google Scholar
[4]	孙新春, 张雨莲, 高永伟. 2011. 甘蒙北山北带古生代地壳演化与成矿作用[J]. 甘肃地质, 20(2): 45−50. Google Scholar
[5]	殷勇, 殷先明. 2010. 花牛山地区中生代A型花岗岩特征及其找矿意义[J]. 甘肃地质, 19(1): 6−14. Google Scholar
[6]	余吉远, 王国强, 李向民, 计波, 闫巧娟. 2015. 北山地区花牛山群的重新厘定−来自火山岩地球化学证据[J]. 新疆地质, 33(4): 537−543. doi: 10.3969/j.issn.1000-8845.2015.04.022 CrossRef Google Scholar
[7]	左国朝, 何国琦. 1990. 北山板块构造及成矿规律[M]. 北京: 北京大学出版社. Google Scholar
[1]	Kröner A, Hegner E, Lehmann B, Heinhorstc J, Wingated MTD, Liue DY, Ermelovf P. 2008. Palaeozoic arc magmatism in the Central Asian Orogenic Belt of Kazakhstan: SHRIMP zircon ages and whole-rock Nd isotopic systematic[J]. Journal of Asian Earth Sciences, 32(2): 118−130. Google Scholar
[2]	Miao Laicheng, Zhu Mingshuai, Zhang Fuqin. 2014. Tectonic setting of Mesozoic magmatism and associated metallogenesis in Beishan area[J]. Geology in China, 41(4): 1191−1204 (in Chinese with English abstract). Google Scholar
[3]	Sun Xinchun, Zhang Yulian, Gao Yongwei. 2011. Paleozolc crustal evolution and mineralization of the northern Beishan in Gansu[J]. Gansu Geology, 20(2): 45−50 (in Chinese with English abstract). Google Scholar
[4]	Xiao WJ, Mao QG, Windley BF, et al. 2010. Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage[J]. American Journal of Science, 310(10): 1553−1594. Google Scholar
[5]	Yin Yong, Yin Xianming. 2010. Features of mesozoic a-type geanites and it’s significancesfor prospecting in Huaniushan area[J]. Gansu Geology, 19(1): 6−14 (in Chinese with English abstract). Google Scholar
[6]	Yu Jiyuan, Wang Guoqiang, Li Xiangmin, Ji Bo, Yan Qiaojuan. 2015. The Redefinition of Huaniushan Group in Beishan area: Geochemical Evidence from Volcanic Rocks[J]. Xinjiang Geology, 33(4): 537−543 (in Chinese with English abstract). Google Scholar
[7]	Zuo Guochao, He Guoqi. 1990. Beishan plate structure and metallogenic regularity [M].Beijing: Peking University Press (in Chinese). Google Scholar