[1] XIE R H, XIAO L Z. The (T2, D) NMR logging method for fluids characterization[J]. Chinese Journal of Geophysics, 2009, 52(9):2410-2418.谢然红, 肖立志. (T2, D)二维核磁共振测井识别储层流体的方法[J]. 地球物理学报, 2009, 52(9):2410-2418. [2] SHAO W Z. On effect of NMR differential and shifted spectrum method in laboratory[J]. Well Logging Technology, 2004, 27(6):502-507.邵维志. 核磁共振测井移谱差谱法影响因素实验分析[J]. 测井技术, 2004, 27(6):502-507. [3] HU F L, ZHOU C C, LI C L, et al. Fluid identification method based on 2D diffusion-relaxation nuclear magnetic resonance (NMR)[J]. Petroleum exploration and developmen, 2012, 39(5):552-558.胡法龙, 周灿灿, 李潮流, 等. 基于弛豫-扩散的二维核磁共振流体识别方法[J]. 石油勘探与开发, 2012, 39(5):552-558. [4] FENG D J, ZHU T, LI H T. Geological features and control factors of reservior forming in middle Triassic Leikoupo Formation in western Sichuan Basin[J].Jouranal of Xi'an shiyou university(Natural science edition), 2013, 28(6):1-7.冯动军, 朱彤, 李宏涛. 川西海相雷口坡组成藏地质特征及控制因素[J]. 西安石油大学学报(自然科学版), 2013, 28(6):1-7. [5] CHENG J J. Application of NMR log data to productivity evaluation of tight sandstone gas reserviors[J]. Offshore oil, 2017, 37(4):57-62.成家杰. 核磁测井资料在致密砂岩储层产能评价中的应用[J]. 海洋石油, 2017, 37(4):57-62. [6] DING Y J, CAI X Y, SHAO W Z, et al. Key parameters of water saturation based on concentration of T2 sprctrum distribution[J]. Well logging technology, 2017, 41(4):405-411.丁娱娇, 柴细元, 邵维志, 等. 基于核磁共振T2谱集中度的低孔隙度低渗透率储层饱和度参数研究[J]. 测井技术, 2017, 41(4):405-411. [7] ZHANG S M, ZHANG S N, GE X, et al. Optimal design and application of two-dimensional NMR logging in Chuanxi Tight Gas Reservoir[J]. Chinese J Magn Reson, 2018, 35(2):234-242.张世懋, 张哨楠, 葛祥, 等. 川西致密气藏二维核磁共振测井优化设计与应用[J]. 波谱学杂志, 2018, 35(2):234-242 [8] HOU K J, WU J M, GE X, et al. Porosity computational method based on 2D NMR relaxation spectra of leikoupo group's 4th section in western Chuanxi[J]. Chinese J Magn Reson, 2020, 37(2):162-171.侯克均, 吴见萌, 葛祥, 等. 基于二维核磁共振弛豫谱的川西雷四段孔隙度计算方法[J]. 波谱学杂志, 2020, 37(2):162-171. [9] HAYASHI S, AKIBA E. Nuclear spin-lattice relaxation mechanisms in kaolinite confirmed by magic-angle spinning[J]. Solid State Nucl Magn, 1995, 4(6):331-340. [10] HÜRLIMANN M D. Effective gradients in porous media due to susceptibility differences[J]. J Magn Reson, 1998, 131(2):232-240. [11] HÜRLIMANN M D. Diffusion and relaxation effects in general stray field NMR experiments[J]. J Magn Reson, 2001, 148(2):367-378. [12] ITSKOVICH G, REIDERMAN A. Method and apparatus for multi-frequency NMR diffusion measurements in the presence of internal magnetic field gradients:US, US7049815[P]. 2006. [13] CHITALE D V, COATES G R, DAY P I, et al. System and method for clay typing using nmr-based porosity modeling:US, US 6646437 B1[P]. 2003. [14] HAGIWARA T. NMR Logging using time-domain averaging:US, US7135862[P]. 2006. [15] DUNN K J, Latorraca G A. The inversion of NMR log data sets with different measurement errors[J]. J Magn Reson, 1999, 140(1):153-161. [16] MENG X N, XIE R H, LI C X, et al. An NMR log echo data de-noising method based on the wavelet packet threshold algorithm[J]. J Geophys Eng, 2015, 12(6):956-968. |