“Honggeertu volcanic field”的意思、由来-开放百科全书

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Honggeertu volcanic field

释义

References
External links

{{coord|41.47|N|113|E|display=intitle|notes=^[1]}}Honggeertu is a volcanic field in China, in the Nei Mongol Province.^[1]

The field is formed by twelve basaltic cinder cones.^[1] Some of the cones formed on a fault.^[4] It may be of Holocene age.^[1] Young lava flows from this field look much younger than these of Quaternary volcanoes in the neighbourhood.^[6] The volcanism may originate in the tectonic effects of the movement of the Ordos Block. Seismic tomography indicates the presence of a low velocity region at the volcano.

References

1. ^¹{{cite journal|last1=Whitford-Stark|first1=J. L.|title=A survey of Cenozoic volcanism on mainland Asia|volume=213|year=1987|pages=1–74|issn=0072-1077|doi=10.1130/SPE213-p1}}
2. ^¹²³⁴{{Cite GVP|vn=305010|name=Honggeertu}}
3. ^¹{{cite journal|last1=Wei|first1=H.|last2=Sparks|first2=R.S.J.|last3=Liu|first3=R.|last4=Fan|first4=Q.|last5=Wang|first5=Y.|last6=Hong|first6=H.|last7=Zhang|first7=H.|last8=Chen|first8=H.|last9=Jiang|first9=C.|last10=Dong|first10=J.|last11=Zheng|first11=Y.|last12=Pan|first12=Y.|title=Three active volcanoes in China and their hazards|journal=Journal of Asian Earth Sciences|date=February 2003|volume=21|issue=5|page=516|doi=10.1016/S1367-9120(02)00081-0}}

^[1]^[2]^[3]
}}

External links

Petrogenesis and tectonic setting of the granites in Honggeertu area, central Inner Mongolia：Constraints from LA-ICP-MS zircon U-Pb chronology and geochemistry

2 : Volcanoes of China|Quaternary volcanism

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