李斌, 史晓颖, 程长青, 郭彦如. 空间数据库技术在定量单因素作图法中的应用——以鄂尔多斯盆地奥陶系SQ17岩相古地理研究为例[J]. 煤田地质与勘探, 2010, 38(1): 1-6. DOI: 10.3969/j.issn.1001-1986.2010.01.001
引用本文: 李斌, 史晓颖, 程长青, 郭彦如. 空间数据库技术在定量单因素作图法中的应用——以鄂尔多斯盆地奥陶系SQ17岩相古地理研究为例[J]. 煤田地质与勘探, 2010, 38(1): 1-6. DOI: 10.3969/j.issn.1001-1986.2010.01.001
LI Bin, SHI Xiaoying, CHENG Changqing, GUO Yanru. Application of spatial database and single-factor analysis in litho-palaeogeographic reconstruction of the Ordos basin[J]. COAL GEOLOGY & EXPLORATION, 2010, 38(1): 1-6. DOI: 10.3969/j.issn.1001-1986.2010.01.001
Citation: LI Bin, SHI Xiaoying, CHENG Changqing, GUO Yanru. Application of spatial database and single-factor analysis in litho-palaeogeographic reconstruction of the Ordos basin[J]. COAL GEOLOGY & EXPLORATION, 2010, 38(1): 1-6. DOI: 10.3969/j.issn.1001-1986.2010.01.001

空间数据库技术在定量单因素作图法中的应用——以鄂尔多斯盆地奥陶系SQ17岩相古地理研究为例

Application of spatial database and single-factor analysis in litho-palaeogeographic reconstruction of the Ordos basin

  • 摘要: 对野外剖面记录、测井和录井资料等海量空间数据的对比分析是层序岩相古地理研究的根本途径。应用空间数据库技术与单因素分析作图法相结合,将鄂尔多斯奥陶系基础地质数据以自然层为单位,按照统一标准定量化处理,并利用空间数据库技术系统管理。然后,以层序为单位计算、统计和分析,进而提取厚度、含量(如白云岩和陆源物等含量)、平均颜色值和准层序个数等反映沉积环境和特征的单因素;定量绘制出各单因素等值线图;在区域地质背景下,通过单因素叠加、多因素综合分析等方法绘制古地理图。以鄂尔多斯盆地奥陶系马五组底部SQ17层序为例,有效地识别出其古地理单元,提高了研究的精度与可靠性。实践证明,空间数据库技术与单因素作图法相结合,是岩相古地理研究的一种有效技术途径,并可推广使用。

     

    Abstract: In the study of sequence stratigraphy and litho-palaeogeography,quantitative analysis,precise calculation and detailed comparison of tremendous geological data,such as field profiles,logging records and artificial seismic curves from different areas,are the basic requirements.In order to obtain more reliable and precise result,we have developed a method,by combining the spatial database analysis and the single-factor mapping technology,to establish sequence stratigraphical succession and to map the Ordovician litho-paleogeography of the Ordos basin-one of the largest oil-gas bearing basin in North China Platform.By using the method,all of the related basic geological data can be quantitatively analyzed and scientifically managed.Various attributes of the basic stratigraphic units and their characters,such as the overall color,sequence and parasequence thickness,pene-contemporaneous dolostone content,shallow water plaster content,terrigenous material content,carbonate grain ratio,parasequence number,and the relative thickness of the lower and upper units in a parasequence,can be fully utilized statistically in facie analysis and in mapping.Based on this analysis,we have exerted single-factor isopachous mapping quantitatively for each of the Ordovician sequences in the basin,and finally synthezed multiple factors to construct the litho-palaeogeographical maps for each of the sequence intervals.The study shows that the proposed method is quite effective and has much higher resolution in recognizing litho-paleogeographic units than traditional ways.For example,in one of the Middle Ordovician sequence interval(the SQ17 in Lower Majiagou Formaton) of the Ordos basin,we have successfully mapped the precise distribution of various facie units.

     

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