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Central Shandong, Changle County, Weifang, Shandong, Chinai
Regional Level Types
Central ShandongVolcanic Range
Changle CountyCounty
WeifangPrefecture-level City
ShandongProvince
ChinaCountry

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PhotosMapsSearch
Key
Latitude & Longitude (WGS84):
36° 25' North , 118° 55' East
Latitude & Longitude (decimal):
Locality type:


In the central area of Shandong Province are two lines of NE-SW-trending basaltic volcanoes, each c.40km in length. The more northerly line includes the volcanoes of Niushan, Shanwang, Taohuashan, Fangshan and Fuyanshan and the southern the Longshan, Chendingshan and Liushan volcanoes.

Select Mineral List Type

Standard Detailed Strunz Dana Chemical Elements

Mineral List


1 valid mineral.

Rock Types Recorded

Note: this is a very new system on mindat.org and data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

'Albite-Anorthite Series'
Reference: Zeng, G., Chen, L. H., Xu, X. S., Jiang, S. Y., & Hofmann, A. W. (2010). Carbonated mantle sources for Cenozoic intra-plate alkaline basalts in Shandong, North China. Chemical Geology, 273(1-2), 35-45. Chen, Y., Zhang, Y., Graham, D., Su, S., & Deng, J. (2007). Geochemistry of Cenozoic basalts and mantle xenoliths in Northeast China. Lithos, 96(1-2), 108-126.
'Fayalite-Forsterite Series'
Reference: Zeng, G., Chen, L. H., Xu, X. S., Jiang, S. Y., & Hofmann, A. W. (2010). Carbonated mantle sources for Cenozoic intra-plate alkaline basalts in Shandong, North China. Chemical Geology, 273(1-2), 35-45. Chen, Y., Zhang, Y., Graham, D., Su, S., & Deng, J. (2007). Geochemistry of Cenozoic basalts and mantle xenoliths in Northeast China. Lithos, 96(1-2), 108-126.
'Glass'
Reference: Zeng, G., Chen, L. H., Xu, X. S., Jiang, S. Y., & Hofmann, A. W. (2010). Carbonated mantle sources for Cenozoic intra-plate alkaline basalts in Shandong, North China. Chemical Geology, 273(1-2), 35-45. Chen, Y., Zhang, Y., Graham, D., Su, S., & Deng, J. (2007). Geochemistry of Cenozoic basalts and mantle xenoliths in Northeast China. Lithos, 96(1-2), 108-126.
Magnetite
Formula: Fe2+Fe3+2O4
Reference: Zeng, G., Chen, L. H., Xu, X. S., Jiang, S. Y., & Hofmann, A. W. (2010). Carbonated mantle sources for Cenozoic intra-plate alkaline basalts in Shandong, North China. Chemical Geology, 273(1-2), 35-45. Chen, Y., Zhang, Y., Graham, D., Su, S., & Deng, J. (2007). Geochemistry of Cenozoic basalts and mantle xenoliths in Northeast China. Lithos, 96(1-2), 108-126.
Magnetite var: Titaniferous Magnetite
Formula: Fe2+(Fe3+,Ti)2O4
Reference: Zeng, G., Chen, L. H., Xu, X. S., Jiang, S. Y., & Hofmann, A. W. (2010). Carbonated mantle sources for Cenozoic intra-plate alkaline basalts in Shandong, North China. Chemical Geology, 273(1-2), 35-45. Chen, Y., Zhang, Y., Graham, D., Su, S., & Deng, J. (2007). Geochemistry of Cenozoic basalts and mantle xenoliths in Northeast China. Lithos, 96(1-2), 108-126.
'Pyroxene Group'
Reference: Zeng, G., Chen, L. H., Xu, X. S., Jiang, S. Y., & Hofmann, A. W. (2010). Carbonated mantle sources for Cenozoic intra-plate alkaline basalts in Shandong, North China. Chemical Geology, 273(1-2), 35-45. Chen, Y., Zhang, Y., Graham, D., Su, S., & Deng, J. (2007). Geochemistry of Cenozoic basalts and mantle xenoliths in Northeast China. Lithos, 96(1-2), 108-126.

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Magnetite4.BB.05Fe2+Fe3+2O4
var: Titaniferous Magnetite4.BB.05Fe2+(Fe3+,Ti)2O4
Unclassified Minerals, Rocks, etc.
'Albite-Anorthite Series'-
'Fayalite-Forsterite Series'-
'Glass'-
'Pyroxene Group'-

List of minerals arranged by Dana 8th Edition classification

Group 7 - MULTIPLE OXIDES
AB2X4
Magnetite7.2.2.3Fe2+Fe3+2O4
Unclassified Minerals, Mixtures, etc.
'Albite-Anorthite Series'-
'Fayalite-Forsterite Series'-
'Glass'-
Magnetite
var: Titaniferous Magnetite
-Fe2+(Fe3+,Ti)2O4
'Pyroxene Group'-

List of minerals for each chemical element

OOxygen
O Magnetite (var: Titaniferous Magnetite)Fe2+(Fe3+,Ti)2O4
O MagnetiteFe2+Fe23+O4
TiTitanium
Ti Magnetite (var: Titaniferous Magnetite)Fe2+(Fe3+,Ti)2O4
FeIron
Fe Magnetite (var: Titaniferous Magnetite)Fe2+(Fe3+,Ti)2O4
Fe MagnetiteFe2+Fe23+O4

Geochronology

Mineralization age: Cenozoic : 24.0 Ma to 0.3 Ma

Important note: This table is based only on rock and mineral ages recorded below and is not necessarily a complete representation of the geochronology, but does give an indication of possible mineralization events relevant to this locality. As more age information is added this table may expand in the future. A break in the table simply indicates a lack of data entered here, not necessarily a break in the geologic sequence. Grey background entries are from different, related, localities.

Geologic TimeRocks, Minerals and Events
Phanerozoic
 Cenozoic
  Quaternary
   Pleistocene
ⓘ Basalt (youngest age)0.3 Ma
    
   
  Paleogene
   Oligocene
ⓘ Basalt (oldest age)24.0 Ma

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Woolley A.R. (2019) Alkaline Rocks and Carbonatites of the World. Part 4: Antarctica, Asia and Europe, p.69
Zeng, G., Chen, L. H., Xu, X. S., Jiang, S. Y., & Hofmann, A. W. (2010). Carbonated mantle sources for Cenozoic intra-plate alkaline basalts in Shandong, North China. Chemical Geology, 273(1-2), 35-45.
Zeng, G., Chen, L. H., Hofmann, A. W., Jiang, S. Y., & Xu, X. S. (2011). Crust recycling in the sources of two parallel volcanic chains in Shandong, North China. Earth and Planetary Science Letters, 302(3-4), 359-368.

Other Regions, Features and Areas containing this locality

AsiaContinent
Eurasian PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.
 
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