|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | 吕梁山隆升时限与演化过程研究显示文摘对吕梁山地区中-新生代隆升时限及其演化的认识,是恢复鄂尔多斯盆地沉积东界的基础,也是探讨华北克拉通演化和破坏等科学问题的有机组成部分.本文以盆山耦合的研究思路为指导,通过较系统的裂变径迹热年代学采样分析,认为吕梁山地区显生宙的隆升活动主要发生在早白垩世晚期以来,可进一步分为缓慢抬升(120~65 Ma)、加速抬升(65~23 Ma)及强烈抬升(23 Ma以来)3个隆升演化阶段,新生代以来是其最主要的隆升时期.抬升作用在空间上具非均衡性,中、北部抬升早,南部晚.晚新生代以来吕梁山地区的快速隆升作用,与东部相邻断陷的沉降具有成因耦合联系.吕梁山地区晚中生代-新生代以来的隆升演化,可能主要与青藏高原挤压造山作用和太平洋板块俯冲的远程效应有关. | 赵俊峰 刘池洋 Nigel MOUNTNEY 芦建军 曹冀龙 杨瑶 薛锐 | 2015 | 中国科学:地球科学2015，45，10： | 20 |
| 2 | Timing of uplift and evolution of the Lüliang Mountains,North China Craton显示文摘This study analyses evidence for reformed basin development and basin-mountain coupling associated with development of the Ordos Basin and the Lüliang Mountains, China. Gaining an improved understanding of the timing and nature of uplift and evolution of the Lüliang Mountains is important for the reconstruction of the eastern sedimentary boundary of the Ordos Basin(a major petroliferous basin) as well as for providing insight into the evolution and breakup of the North China Craton(NCC). Based on systematic sampling for fission track analysis, it is suggested that the main phase of uplift of the Lüliang Mountains occurred since later part of the Early Cretaceous. Three evolutionary stages of uplift and development are identified: slow initial uplift(120–65 Ma), accelerated uplift(65–23 Ma), and intensive uplift(23 Ma to present), with the majority of the uplift activity having occurred during the Cenozoic. The history of uplift is non-equilibrium and exhibits complexity in temporal and spatial aspects. The middle and northern parts of the Lüliang Mountains were uplifted earlier than the southern part. The most intensive episode of uplift activity commenced in the Miocene and was associated with a genetic coupling relationship with the eastern neighboring Cenozoic Shanxi Grabens. The uplifting and evolutionary processes of the Lüliang Mountains area since later part of the Early Cretaceous share a unified regional geodynamic setting, which was accompanied by uplift of the Mesozoic Ordos Basin and development of the neighboring Cenozoic Shanxi Grabens. Collectively, this regional orogenic activity is related principally to the far-field effects of both the compression sourced from the southwestern Tibet Plateau and westward subduction of the Pacific Plate in Cenozoic. | ZHAO JunFeng LIU ChiYang Nigel MOUNTNEY LU JianJun CAO JiLong YANG Yao XUE Rui | 2016 | Science China Earth Sciences2016，59，1： | 2 |
| 3 | Original Sedimentary Pattern of an Inverted Basin:A Case Study from the Bozhong Depression,Offshore Bohai Bay Basin显示文摘The third member of Shahejie Formation(Sha-3 member; 42–38Ma of Eocene) in the Bozhong Depression,offshore Bohai Bay Basin was subject to multiple post-depositional modifications. The present structural framework of the Bozhong Depression,which is characterized by sags alternating with uplifts,does not reflect its original sedimentary pattern. Previous studies have not discussed the post-depositional modification of this succession,including the sedimentary pattern variations and the depositional geodynamic setting. This work determined the characteristics of the post-depositional modification and original sedimentary pattern of the Bozhong Depression through analysis of seismic data,well-log data and fission-track ages. The results demonstrate that the Shijiutuo rise,a major structural feature of the current basin,did not exist during the major depositional stage of the Sha-3 member,when the Qinnan sag was largely connected to the Bozhong sag to form a single contiguous deposition area within the basin. By contrast,the Shaleitian and Chengbei rises,located in the western part of the Bozhong Depression,have existed before the depositional period of the Eocene Sha-3 member; these features were manifested as syn-depositional tilted fault blocks,the uplifted footwall blocks of which provided sediments for the neighboring Shanan and Chengbei sags. The western part of the Bonan low rise,located in the southern part of the Bozhong Depression,did not experience uplifting during the depositional phase of the Eocene Sha-3 member. The Huanghekou sag was connected with the Bozhong sag in the western part of the Bozhong Depression. The original sedimentary boundary of the southern Miaoxi sag possibly extended eastward about 10 km and connected with the Bozhong sag at its northern part. The present-day Bodong low rise,which is bounded by the Tan–Lu fault zone,also formed after the depositional period of Eocene Sha-3 member. It is thus concluded that the Bozhong Depression formed a connected large-scale sub-basin during the depositional stage of the Eocene Sha-3 member. Several neighboring sags that are now separated by rises,including the Qinnan,Shanan,Chengbei,Huanghekou,Miaoxi and Bodong sags,formed a single contiguous depositional area during the Eocene. The significant differences between the present and original basin patter and framework provide valuable information for better understanding the history of basin inversion and its impact on related hydrocarbon-system evolution. | ZHAO Junfeng LIU Chiyang HUANG Lei MOUNTNEY Nigel HAN Shaojia LIU Peng HU Junhao | 2016 | Acta Geologica Sinica(English Edition)2016，90，6： | 2 |
| 4 | Aeolian architecture, bedform climbing and preservation space in the Cretaceous Etjo Forma- tion, NW Namibia显示文摘 | Mountney N P Howell J A | 2002 | Sedimentology2002，49，： | 1 |
| 5 | Tensile strength of the medial patellofemoral ligament before and after repair or recon- struction显示文摘 | Mountney J Senavongse W Amis AA | 2005 | J Bone Joint Surg Br2005，87，1： | 1 |
| 6 | Aeolian architecture, bedform climbing and preservation space in the Cretaceous Etjo Formation, NW Namibia显示文摘 | Mountney N P Howell J A | 2002 | Sedimentology2002，47，： | 1 |
| 7 | Anatomy andbiomechanics of the medial patellofemoral ligament显示文摘 | Amis AA Firer P Mountney J et al | 2003 | Knee2003，10，21： | 1 |
| 8 | Anatomy and biomechanics of the medial patellofemoral ligament显示文摘 | Amis AA Firer P Mountney J | 2003 | Knee2003，10，3： | 1 |
| 9 | A novel animal model of closed - head concussive - induced mild trau- matic brain injuy : development, implementation, and characterization显示文摘 | Chen Z leung LY Mountney A | 2012 | J Neurotrauma2012，29，2： | 1 |
| 10 | When is a meniscal cyst not a meniscal cyst显示文摘 | Mountney J Thomas NP | 2004 | Knee2004，11，2： | 1 |
| 11 | Prevention of postoperative wound haematomas and hyperperfusion following carotid endarterectomy显示文摘 | Mountney J Wilkinson JM | 2001 | Eur J Vasc Endovasc Surg2001，21，： | 1 |
| 12 | Neuroprotective effects of sulforaphane after contusive spinal cord injury 显示文摘 | Benedict AL Mountney A Hurtado A | 2012 | J Neurotrauma2012，29，16： | 1 |
| 13 | Tensile strength of the medial patellofemoral ligament before and after repair or reconstruction 显示文摘 | Mountney J Senavongse AA Amis AA et al | 2005 | J Bone Joint Surg2005，87，1： | 1 |
| 14 | Anatomy and biomechanics of the medial patenofemoral ligament 显示文摘 | Amis AA Firer P Mountney J | 2003 | Knee2003，0，： | 1 |
| 15 | Anatomy and biomechanics of the medial patellofemoral ligament显示文摘 | Amis AA Firer P Mountney J | 2003 | Knee2003，3，： | 1 |
| 16 | Optical techniques for 3D surface reconstruction in computer-assisted laparoscopic surgery显示文摘 | Maierhein L Mountney P Bartoli A | 2013 | Medical image analysis2013，17，8： | 1 |
| 17 | Anatomy and biomechanics of the medial patellofemoral ligament显示文摘 | Amis AA Firer P Mountney J | 2003 | Knee2003，10，2： | 1 |
| 18 | Anatomy and biome- chanics of the medical patellofemoral ligament显示文摘 | Amis AA Firer P Mountney J | 2003 | Knee2003，10，3： | 1 |
| 19 | Three-Dimensional Tissue Deformation Recovery and Tracking:Introducing Techniques Based on Laparoscopic or Endoscopic hnages显示文摘 | MOUNTNEY P STOYANOY D YANG G Z | | 0，，04： | 1 |
| 20 | Tensile strength of the medial patel ofemoral ligament before and after repair or reconstruction显示文摘 | Mountney J Senavongse W Amis AA | | 0，，01： | 1 |
您所在的机构暂未开通此部分的功能，请联系管理员