[1] 王清晨,从柏林,马力. 大别造山带与合肥盆地的构造耦合[J].科学通报,1997,42(6):575~580
[2] 周进高,赵宗举,邓红婴. 合肥盆地构造演化及含油气性分析[J].地质学报,1999,13(1):15~23
[3] 曹高社,李学田,刘德良,等.合肥盆地与北淮阳构造带印支期的推覆构造及其油气意义[J].石油与天然气地质,2003,24(2):116~122
[4] 孙晓猛,张梅生,龙胜祥,等. 秦岭-大别造山带北部逆冲推覆构造与合肥盆地、周口坳陷控盆断裂[J].石油与天然气地质,2004,25(2):191~198
[5] 李丕龙,李学田,宋明水,等. 合肥盆地石油地质与地球物理特征研究及进展[M].北京:地质出版社,2003.88~179
[6] 薛爱民,金维浚. 合肥盆地油气地质及其与大别造山带构造耦合[M].北京:石油工业出版社,2001. 36~103
[7] 陈刚,李丕龙,李学田. 合肥盆地原型恢复与油气评价的研究方法思考[J].石油实验地质,2002,24(3):200~203
[8] 胡圣标,汪集旸.沉积盆地热体制研究的基本原理和进展[J]. 地学前缘,1995,2(3~4):171~180
[9] 罗晓容. 沉积盆地数值模型的概念、设计及检验[J].石油与天然气地质,1998,19(3):196~204
[10] 周中毅,潘长春. 沉积盆地古地温测定方法及其应用[M].广州:广东科技出版社,1992.1~103
[11] Suggate R P. Relations between depth of burial, vitrinite reflectance and geothermal gradient[J]. Journal of Petroleum Geology, 1998, 21(1):5~32
[12] Barker C E. Temperature and time in the thermal maturation of sedimentary organic mature[A]. In:Naeser N D, McCulloh T H. Thermal history of sedimentary basin-methods and case histories[C]. New York:Springer-Verlag, 1989.73~98
[13] Barker C E. Implications for organic maturation studies and evidence for a geologically rapid increase and stabilization of vitrinite reflectance at peak temperature:Cerro Prieto geothermal system, Mexico[J].AAPG Bull, 1991, 75:1852~1863
[14] 何生,王青玲.关于镜质体反射率恢复地层剥蚀厚度的问题讨论[J]. 地质论评,1989,35(2):120~125
[15] 任战利. 中国北方沉积盆地热演化史的对比[J].石油与天然气地质,2000,21(1):33~37
[16] 肖贤明,刘祖发,申家贵,等. 确定含油气盆地古地温梯度的一种新方法--镜质组反射率梯度法[J]. 科学通报,1998,43(21):2340~2343
[17] 陈刚,赵重远,李丕龙,等. Ro反演的盆地热史恢复方法与相关问题[J].石油与天然气地质,2002,23(4):345~346
[18] Barker C E,Pawlewicz M J.The correlation of vitrinite reflectance with maximum temperature in humic organic mature[A].In:Buntebarth G, Stegena L.Paleogeothermics[C].Berlin:Springer-Verlag,1986.79~93
[19] Marshall J E A. The Silurian of Saudi Arabia:thermal maturity, burial history and geotectonic environment[J]. Review of Palaeobotany and Palynology, 1995, 89:145~150
[20] 张国伟,张本仁,袁学诚. 秦岭造山带与大陆动力学[M].北京:科学出版社,2001.171~282
[21] Jiang L L, Wu W P, Chu D R, et al. Post-collisional extensional and thrust-nappe structures in northern part of Dabie mountains[J]. Chinese Science Bulletin, 2003, 48(21):2378~2385
[22] Zhu G, Song C Z, Wang D X, et al. Studies on 40Ar/39Ar thermochronology of strike-slip time of the Tan-Lu fault zone and their tectonic implication[J]. Science in China (series D), 2001, 44(11):1002~1008
[23] 林银山,郭福生,辜骏如,等. 北淮阳燕山期岩浆岩地球化学特征及其构造环境[J].中国区域地质,2001,20(1):100~106
[24] 陈廷愚,牛宝贵,刘志刚,等. 大别山腹地燕山期岩浆作用和变质作用的同位素年代学研究及其地质意义[J].地质学报,1991, 65(4):329~336
[25] 简平,马昌前,杨坤光. 大别造山带东部燕山晚期区域变质-岩浆活动与区域构造抬升的同位素地质年代学证据[J].地球科学,1996, 21(5):519~523
[26] 陈江峰,谢智,刘顺生,等.大别造山带冷却年龄的40Ar-39Ar和裂变径迹年龄的测定[J].中国科学(D),1995,25(10):1086~1091
[27] 吴堑虹,刘顺生,Jonckheere R,等. 东大别地区磷灰石裂变径迹年龄的构造意义初析[J].地质科学,2002,37(3):343~349
[28] 杨坤光,马昌前,许长海,等. 北淮阳构造带与大别造山带的差异性隆升[J].中国科学(D辑),1999,29(2):97~103
[29] Reiners P W, Zhou Z Y, Ehlers T A, et al. Post-orogenic evolution of the Dabie Shan, eastern China, from (U-Th)/He and fission-track thermochronology[J].American Journal of Science, 2003, 303:489~518
[30] Grimmer J C, Jonckheere R, Enkelmann E, et al. Cretaceous-Cenozoic history of the Southern Tan-Lu fault zone, apatite fission-track and structural constraints from the Dabieshan (eastern China) [J]. Tectonophysics, 2002, 359(3~4):225~253 |