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Keluo

Keluo Group

Medan gunung api · China · 670 m

Several cones of the Keluo Group are shown in this September 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 22 km across). The volcanic field is located in NE China, and is NW of the Wudalianchi volcanic field.
Several cones of the Keluo Group are shown in this September 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 22 km across). The volcanic field is located in NE China, and is NW of the Wudalianchi volcanic field. · Foto: Satellite image courtesy of Planet Labs Inc., 2018 (https://www.planet.com/).
Tipe
Medan gunung api
Negara
China
Wilayah
Eastern Asia Volcanic Regions / Central East Asia Volcanic Province
Ketinggian
670 m
Koordinat
49.370, 125.920
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Intraplate / Continental crust (> 25 km)
Bentuk lahan
Cluster
Batuan utama
Trachybasalt / Tephrite Basanite
Ringkasan geologi

The Keluo volcanic field in NE China is located near the Russian border, S of the Heilongjiang (Black Dragon) River. Like its better known neighbor to the S, the Wudalianchi volcanic field, it contains many high-potassium basaltic cinder cones. Nanshan cone, located at the southern end of the field N of the Keluo River, may be of historical age, based on its youthful appearance, and Gushan may also be Holocene. Other cones to the NE are of Pleistocene to Tertiary. Cinder cones are located at the intersections of regional NE- and NW-trending lineaments, and were erupted through basement volcanic and sedimentary rocks of Jurassic-Cretaceous age, granitic rocks, and pre-Permian metasediments. There are unconfirmed reports of observed activity.

Ringkasan Wikipedia

Ringkasan Inggris

Keluo is a dormant volcanic field 310 kilometers (190 mi) north-by-northwest of Daquijin in northeastern China. It is located at an intersection of regional lineaments trending northeast and northwest; the volcanoes were erupted through basement igneous and sedimentary rocks from the Jurassic to Cretaceous, through granite, and through pre-Permian metasediments. Like the Wudalianchi volcanic to its south, it contains high-potassium basaltic cinder cones.

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