The Mesoproterozoic ‘seismite’ at Laiyuan (Hebei Province, E China) re-interpreted

• Autorzy: Van Loon A. J.

Identyfikatory

DOI

10.2478/logos-2014-0012

• Języki publikacji: EN

Abstrakty

EN

A 1-million m3 breccia near Laiyuan (Hebei Province, E China) occurs as a block-like lithological unit between dolostones of the 1.55–1.45 Ga (Early Mesoproterozoic) Wumishan Formation. It has previously been interpreted as a seismite, but it appears not to fulfil any of the commonly accepted criteria that jointly are considered diagnostic for seismites. Its presence in a graben-like structure with almost vertical bounding fault planes rather indicates an origin as a (submarine) valley fill. As the valley originated by tectonic activity in the form of faulting, the breccia can be considered as a secondary effect of seismic activity, but it does not represent a seismite.

Słowa kluczowe

EN

seismites; valley-fill; graben sedimentation; Wumishan Formation; Mesoproterozoic; Fangshan geopark; Hebei Province; China

PL

sejsmity; mezoproterozoik; Geopark Fang Shan; prowincja Hebei; Chiny

• Wydawca: Uniwersytet im. Adama Mickiewicza. Instytut Geologii
• Czasopismo: Geologos
• Rocznik: 2014
• Tom: Vol. 20, No. 2
• Strony: 139--146
• Opis fizyczny: Bibliogr. 48 poz.

Twórcy

autor

Van Loon A. J.

• Geological Institute, Adam Mickiewicz University, Maków Polnych 16, 61-606 Poznań, Poland

Bibliografia

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