Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (4): 949-973.doi: 10.13278/j.cnki.jjuese.201704101

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Spatio-Temporal Attributes of Volcano Stratigraphy and Its Lithostratigraphic Units in a Basin

Tang Huafeng1, Zhao Pengjiu1, Gao Youfeng2, Wang Pujun1, Qi Yuning1   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Research Center of Palaeontology & Stratigraphy of Jilin University, Changchun 130026, China
  • Received:2016-12-23 Online:2017-07-26 Published:2017-07-26
  • Supported by:
    Supported by National Key Basic Research Program of China("973" Program)(2012CB822002) and National Science Foundation of China(41472304)

Abstract: Volcano stratigraphy has three distinguishing features:temporal attributes of ephemeral construction and long erosion, spatial attributes controlled by eruption style and paleo-topography, and occurrence changed with volcanic vents. In this paper,the classification and identification marks of bed, deposit unit and volcanic edifices are introduced in detail. Volcano stratigraphic units were determined by using stratigraphic boundary to reflect temporal attributes, and by using lithology succession and geometrical shape to reflect spatial attributes and occurrence characteristics. The stratigraphic units include bed, deposit unit, volcanic edifice, member, formation, and group. The bed was determined by the differences between rock colors, chemical components,and fabrics. According to an eruptive style and emplacement environment, the deposit units were divided into 3 types,namely lava, volcanic clastics,and reworked volcanic clastics. The occurrence changes continuously within a deposit unit, and the units are separated by an eruptive unconformity/eruptive conformity. A volcanic edifice is a product of ordered stacked deposit units. Volcanic strata lean along volcano vents,and their dip angles decrease gradually from central belt to distal belt. Volcanic edifices were divided by eruptive interval unconformity boundary. More attentions should be paid to the spatial attributes so as to establish a volcano stratigraphic framework. The buried history of volcano stratigraphy should base on the analysis of central belt and distal belt of volcanic edifices. On the basis of the new framework of volcano stratigraphic units,the reservoir distribution are more reasonable

Key words: volcanostratigraphic unit, volcanic edifice, deposit unit, spatio-temporal attributes

CLC Number: 

  • P53
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