Xu Wei, Xie Xinong. A new method to calculate sedimentary rates based on Milankovitch Cycles: a case study on middle section of 3rd member of Shahejie Formation in well Niu38, Dongying Sag, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(2): 207-214. doi: 10.11781/sysydz201202207
Citation: Xu Wei, Xie Xinong. A new method to calculate sedimentary rates based on Milankovitch Cycles: a case study on middle section of 3rd member of Shahejie Formation in well Niu38, Dongying Sag, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(2): 207-214. doi: 10.11781/sysydz201202207

A new method to calculate sedimentary rates based on Milankovitch Cycles: a case study on middle section of 3rd member of Shahejie Formation in well Niu38, Dongying Sag, Bohai Bay Basin

doi: 10.11781/sysydz201202207
  • Received Date: 2011-05-17
  • Rev Recd Date: 2012-02-07
  • Publish Date: 2012-03-28
  • A case study was carried out in the middle section of the 3rd member of the Shahejie Formation in well Niu38,Dongying Sag,Bohai Bay Basin.Spectrum analysis and continuous wavelet spectrum of GR log which was closely related to climate change indicated that the target interval was significantly controlled by the eccentricity period of 125 ka corresponding to the thickness of 12.127 m.The filter analysis of this period revealed that about 40 cycles of 125 ka were preserved in the target interval.High-resolution astronomical time scale was established,by means of which the age of the top of the target interval was 33.975 Ma since that of the bottom of the target interval was 38.975 Ma.Based on regional stratigraphic framework,combined with seismic,core and logging data,the Dongying delta was divided into 9 periods named Z1-Z9.According to the sliding window spectrum analysis,the sedimentary rates of the target interval first increased and then decreased as time went by.The sedimentary rate of Z4 reached the maximum (0.127 m/ka) during the most prosperous period of delta prograding.Finally,the duration of each period and more accurate geological age of the interfaces were calculated on the basis of sedimentary rates.

     

  • loading
  • [1]
    Hays J D,Imbrie J,Shackleton N J.Variations in the Earth's orbit:pacemaker of the ice ages[J].Science,1976,194(4270):1121-1132.
    [2]
    Berger A,Loutre M F,Laskar J.Stability of the astronomical frequencies over the earth's history for paleoclimate studies[J].Science New Series,1992,255(5044):560-566.
    [3]
    姚益民,徐旭辉,刘翠荣,等.米氏旋回剥蚀量计算方法在泌阳凹陷的应用[J].石油实验地质,2011,33(5):460-467.
    [4]
    姚益民,徐道一.东营凹陷牛38井沙三段高分辨率旋回地层研究[J].地层学杂志,2007,31(3):229-239.
    [5]
    林会喜,鄢继华.渤海湾盆地东营凹陷古近系沙河街组三段沉积相类型及平面分布特征[J].石油实验地质,2005,27(1):55-61.
    [6]
    Abels H A,Aziz H A,Krijgsman W,et al.Long-period eccentricity control on sedimentary sequences in the continental Madrid Basin(middle Miocene,Spain)[J].Earth and Planetary Science Letters,2010,289:220-231.
    [7]
    Wonik Thomas.Gamma-Ray measurement in the KirchrodeⅠand Ⅱ boreholes[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2001,174:97-105.
    [8]
    测井软件项目组.Forward工程技术手册[M].北京:石油工业出版社,1999.
    [9]
    Schulz M,Mudelsee M.REDFIT:estimatingred-noise spectra directly from unevenly spaced paleoclimatic time series[J].Computers & Geosciences,2002,28:421-426.
    [10]
    Torrence C,Compo G P.A practical guide to wavelet analysis[J].Bulletin of the American Meteorological Society,1998,79(1):61-78.
    [11]
    Sen A K,Filippelli G M,José-Abel F.An application of wavelet analysis to paleoproductivity records from the Southern Ocean[J].Computers & Geosciences,2009,35:1445-1450.
    [12]
    Laskar J,Robutel P,Joutel F,et al.A long-term numericalsolution for the insolation quantities of the Earth[J].Astronomy and Astrophysics,2004,428:261-285.
    [13]
    Hinnov L A,Ogg J G.Cyclostratigraphy and the astronomical time scale[J].Stratigraphy,2007,4:239-251.
    [14]
    Lirer F,Harzhauser M,Pelosi N,et al.Astronomically forced teleconnection between Paratethyan and Mediterranean sediments during the Middle and Late Miocene[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2009,275:1-13.
    [15]
    田军,汪品先,成鑫荣,等.南海ODP1143站上新世至更新世天文年代标尺的建立[J].地球科学——中国地质大学学报,2005,30(1):31-39.
    [16]
    张善文,张林晔.东营凹陷古近系异常高压的形成与岩性油藏的含油性研究[J].科学通报,2009,54(11):1570-1578.
    [17]
    Gorgas T J, Wilkens R H.Sedimentation rates off SW Africa since the late Miocene deciphered from spectral analyses of borehole and GRA bulk density profiles:ODP Sites 1081-1084[J].Marine geology,2002,180:29-47.
    [18]
    吴怀春,张世红,黄清华.中国东北松辽盆地晚白垩世青山口组浮动天文年代标尺的建立[J].地学前缘,2008,15(4):159-169.
    [19]
    王居峰. 济阳坳陷东营凹陷古近系沙河街组沉积相[J].古地理学报,2005,7(1):45-58.
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article views (3975) PDF downloads(1934) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return