[an error occurred while processing this directive] ������� 2011, 30(1) 71-79 DOI:     ISSN: 1004-5589 CN: 22-1111/P

����Ŀ¼ | ����Ŀ¼ | ������� | �߼�����                                                            [��ӡ��ҳ]   [�ر�]
����
��չ����
������Ϣ
Supporting info
PDF(2157KB)
[HTMLȫ��]
�����[PDF]
�����
�����뷴��
�ѱ����Ƽ�������
�����ҵ����
�������ù�����
����
Email Alert
���·���
���������Ϣ
���Ĺؼ����������
����΢��
ɰ��ֲ�
��ɽ����
��ͼ����
���������������
������1
�����2
��ϣ��3
����4
��ǰ��2
PubMed
Article by Dong, F. X. 1
Article by Chen, Y. K. 2
Article by Qu, X. Y. 3
Article by Ji, C. 4
Article by Qu, Q. Z. 2
���밼����ͼ������ɽ�������΢�༰ɰ��ֲ�����
������1, �����2, ��ϣ��3, ����4, ��ǰ��2
1�� ��������ѧԺ��������ѧԺ������130021; 2�� �й�ʯ�ͻ����ɷ����޹�˾���������ֹ�˾������130062; 3�� ���ִ�ѧ�����ѧѧԺ������130061; 4�� ��ɫ�����������ʿ���ֵ��ʵ���( ����) ���޹�˾���Ͼ�210007
ժҪ��

ͨ���������밼����ͼ���������ġ��⾮����������ϣ��о��˸�����ɽ�������΢��������ɰ��չ���������������: ��ͼ�����̨���Ͳ���ҪΪ�����޳���; ��ɽ���鴢��ɻ���Ϊ������ƽԭ���������������ǰԵ����������ֱ��������ӵ�΢�ࡢ�����䱡��ɰ΢�ࡢˮ�·����ӵ�΢���ˮ�·����䱡��ɰ΢��; Ŀ�IJ��У�GI1 �㡢GIV2 ��ɰ�ҷ����ϲGI2 �㡢GIV1 ��ɰ�ҷ����Ϻã���Ƭ״������ֲ���

�ؼ����� ����΢��   ɰ��ֲ�   ��ɽ����   ��ͼ����  
Sedimentary microfacies and sand body distributing character in Qingshankou Formation of Suotu area in Changling sag
DONG Fu-Xiang-1, CHEN Yu-Kui-2, QU Xi-Yu-3, JI Chao-4, QU Qian-Zhong-2
1�� Exploration and Mapping Institute��Changchun Institute of Technology��Changchun 130021��China; 2�� Northeast Branch of SINOPEC��Changchun 130062��China; 3�� College of Earth Sciences��Jilin University��Changchun 130061��China; 4�� East China Mineral Exploration and Development Bureau��Geological Survey ( Group) Co�� Ltd��Nanjing 210007��China
Abstract:

By analyzing the drill core��well logging and seismic profile in Suotu area of Changling sag��Qingshankou Formation sedimentary microfacies and characteristics of sand body distribution in this area are studied�� The result indicated that the Gaotaizi oil layer in Suotu oil field was mainly the delta deposit; the Qingshankou reservoir can be divided into the delta plain subfacies deposition and the delta front subfacies deposition��which developed in distributary channel microfacies��interdistributary thin layer granulated microfacies��underwater distributary channel microfacies and underwater interdistributary thin layer granulated microfacies�� In objective layers��GI1 and GIV2 layers are poorly developed sandstone��but GI2 and GIV1 layers are well developed sandstone in a larger-area lamellar distribution pattern��

Keywords: sedimentary microfacies   sand body distribution   Qingshankou Formation   Suotu area  
�ո�����  �޻�����  ����淢������  
DOI:
������Ŀ:

ͨѶ����:
���߼��:
����Email:

�ο����ף�
�������������
1�� ������1,2, ����1, ����ȫ1, ��ΰ1, ������1, ����1.������˹��ظ��ص����ӳ���������������Է���[J]. �������, 2009,28(4): 491-497
2�� ������1, 2, ��־��1, 2, ����1, 2, ����1.������˹��ؼ�ܫ������6 �Ͳ������΢������[J]. �������, 2010,29(4): 614-639

Copyright by �������