2016, 35(1) 264-274 DOI:     ISSN: 1004-5589 CN: 22-1111/P

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Keywords
Songliao Basin
Wangfu fault depression
Huoshiling Formation
incompatible elements
eruptive stages of volcanostratigraphy
ECS logging
Authors
LI Jian-Hua
QU Wei-Hua
ZHAO Ran-Lei
LIU Hong-Tao
TANG Hua-Feng
PubMed
Article by Li, J. H.
Article by Qu, W. H.
Article by Zhao, R. L.
Article by Liu, H. T.
Article by Tang, H. F.

Constraint of incompatible elements in ECS to comparison of thin layer volcanostrata: a case study of rhyolitic volcanostrata of Huoshiling Formation in Wangfu fault depression��southern Songliao Basin��NE China

LI Jian-Hua, QU Wei-Hua, ZHAO Ran-Lei, LIU Hong-Tao, TANG Hua-Feng

1. College of Earth Sciences��Jilin University��Changchun 130061��China; 2. PetroChina Jilin Oilfield Company��Songyuan 138000��Jilin��China

Abstract��

The cross- plot of Gd and Ti of ECS (Elemental Capture Spectroscopy) well logging data is used to contrast the volcanic layers�� The results show that the rhyolitic volcanic layer in Wangfu fault depression can be di- vided into 5 stratigraphic units�� The CS13 and CS14 wells with obvious break- in periods reveal that the characteris- tics of Ti is high in later eruption stage�� so the volcanic eruptive sequence is the stages: 1- 2- 3�� The volcanic activi- ty migrated from south to north��with the eruptive strength from weak (eruptive stage1) to strong (eruptive stage 2) and then to weak (eruptive stage3) in sequence�� The reservoir quality in descending order is eruptive stage 2- 1- 3 according to the relationship between the porosity and permeability of logging and the eruptive stages��and the distribution of favorable reservoir is in the eruptive stage 2��

Keywords�� Songliao Basin   Wangfu fault depression   Huoshiling Formation   incompatible elements   eruptive stages of volcanostratigraphy   ECS logging  
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