全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

甘肃张掖地区白垩系风成砂岩沉积序列!祁连山白垩纪隆升的沉积学响应

, PP. 143-156

Keywords: 风成砂岩,沉积序列,张掖地区,白垩纪,沉积学响应,祁连山隆升

Full-Text   Cite this paper   Add to My Lib

Abstract:

白垩纪祁连山隆升过程及其沉积学响应的研究,对认识青藏高原的形成及其环境效应具有重要意义。受控于祁连山隆升过程的甘肃张掖地区下白垩统,包括赤金堡组、下沟组和中沟组,其基本特征是:(1)分布局限而且厚度上千米的赤金堡组,主要由旋回性发育的“冲积扇(或洪积扇—辫状河—滨湖相风成沙丘”序列所组成,形成一种反映了“雨影效应”的粗碎屑岩序列;(2)下沟组总体为一套红层沉积,在盆地边缘发育更多的风成沙丘,可能代表了与祁连山更加快速隆升相对应的更加强烈的“雨影效应”时期的产物;(3)中沟组,从冲积体系演变为一个分布广泛的湖泊沉积体系,总体上属于潮湿气候背景下未受到“雨影效应”影响的产物,与祁连山均衡抬升存在成因联系;(4)研究区上白垩统总体缺失,可能与祁连山的卸载过程产生的山前地壳均衡反弹存在关联。因此,从赤金堡组到下沟组的风成砂岩序列、特殊的沉积相构成及其演化序列,不但成为窥视早白垩世祁连山隆升过程的物质记录,而且为早白垩世东亚大气环流格局的重建提供了另外一个重要的物质记录。

References

[1]  安芷生,张培震,王二七,等. 2006. 中新世以来我国季风—干旱环境演化与青藏高原的生长[J]. 第四纪研究, 26(5): 678-693
[2]  崔晓庄,江新胜,伍皓,等. 2012. 青藏高原东缘盐源盆地古近纪风成沙丘及其古地理意义[J]. 古地理学报, 14(5): 571-582
[3]  甘肃省地质矿产局. 1989. 甘肃省区域地质志[M]. 北京:地质出版社,1-692
[4]  江新胜,潘忠习. 2005. 中国白垩纪沙漠与气候[M]. 北京:地质出版社,1-117
[5]  江新胜,蔡习尧,潘忠习,等. 2009. 塔里木盆地西南部早白垩世风成沙丘古风向测量与古风带恢复[J]. 沉积与特提斯地质, 29(4): 1-4
[6]  江新胜,崔晓庄,伍皓,等. 2012. 青藏高原东缘古近纪沙漠及其对季风起源的启示[J]. 沉积与特提斯地质, 32(3): 54-63
[7]  王成善,曹珂,黄永健. 2009a. 沉积记录与白垩纪地球表层系统变化[J]. 地学前缘, 16(5): 1-14
[8]  王成善,戴紧根,刘志飞,等. 2009b. 西藏高原与喜马拉雅的隆升历史和研究方法:回顾与进展[J]. 地学前缘, 16(3): 1-30
[9]  王成善,郑和荣,冉波,等. 2010. 活动古地理重建的实践与思考:以青藏特提斯为例[J]. 沉积学报, 28(5): 849-860
[10]  王崇孝,马国福,周在华. 2005. 酒泉盆地中、新生代构造演化及沉积充填特征[J]. 石油勘探与开发, 32(1): 33-36
[11]  伍皓,崔晓庄,熊国庆,等. 2011. 甘肃皋兰—白银—靖远地区早白垩世沙漠沉积的特征及其古风带恢复[J]. 地质通报, 30(7): 1077-1084
[12]  许欢,柳永清,旷宏伟等. 2013. 华北晚侏罗世—早白垩世风成砂沉积及其古地理和古生态学意义[J]. 古地理学报, 15(1): 11-30
[13]  许志琴,蔡志慧,张泽明,等. 2008a. 喜马拉雅东构造结南迦巴瓦构造及组构运动学[J]. 岩石学报, 24(7): 1463-1477
[14]  许志琴,李海兵,唐哲民,等. 2011a. 大型走滑断裂对青藏高原地体构架的改造[J]. 岩石学报, 27(11): 3157-3170
[15]  许志琴,李廷栋,杨经绥,等. 2008b. 大陆动力学的过去、现在和未来:理论与应用[J]. 岩石学报, 24(7): 1433-1444
[16]  Catuneanu O,Abreu V,Bhattacharya J P, et al. 2009. Towards the standardization of sequence stratigraphy[J]. EarthScience Reviews, 92: 1-33
[17]  Ghazi S,Mountney N P. 2009. Facies and architectural element analysis of a meandering fluvial succession:The Permian Warchha Sandstone,Salt Range,Pakistan[J]. Sedimentary Geology, 221: 99-126
[18]  Gibling M R,Tandon S K,Sinha R, et al. 2005. Discontinuitybounded alluvial sequences of the southern Gangetic Plains,India:Aggradation and degradation in response to monsoonal strength[J]. Journal of Sedimentary Research, 75: 369-385
[19]  Hajek E A,Heller P L. 2012. Flowdepth scaling in alluvial architecture and nonmarine sequence stratigraphy:Example from the Castlegate sandstone,central Utah,U.S.A.[J]. Journal of Sedimentary Research, 82: 121-130
[20]  Hallam A. 1985. A review of Mesozoic climates[J]. Journal of the Geological Society(London), 142: 433-445
[21]  Holbrook J M,Scott R W,ObohIkuenobe F E. 2006. Baselevel buffers and buttresses:A model for upstream versus downstream control on fluvial geometry and architecture within sequences[J]. Journal of Sedimentary Research, 76: 162-174
[22]  Holz M,Kalkreuth W,Banerjee Ⅰ. 2002. Sequence stratigraphy of paralic coal-bearing strata:An overview[J]. International Journal of Coal Geology, 48: 147-179
[23]  李海兵,杨经绥. 2004. 青藏高原北部白垩纪隆升的证据[J]. 地学前缘, 11(4): 345-359
[24]  刘东生,郑绵平,郭正堂. 1998. 亚洲季风系统的起源和发展及其与两极冰盖和区域构造运动的时代耦合性[J]. 第四纪研究, 18(3): 194-203
[25]  梅冥相,苏德辰. 2013. 青藏高原隆升的沉积学响应:来自甘肃酒泉地区新生代风成砂岩的启示[J]. 古地理学报, 15(3): 351-361
[26]  梅冥相,于炳松,靳卫广. 2004. 塔里木盆地库车坳陷白垩纪层序地层格架及古地理演化[J]. 古地理学报, 6(3): 261-178
[27]  潘良云,谢结来,李明杰,等. 2006. 酒泉盆地白垩纪—新生代区域构造演化与油气勘探[J]. 石油与天然气地质, 27(1): 62-69
[28]  施雅风,李吉均,李炳元,等. 1999. 晚新生代青藏高原的隆升与东亚环境变化[J]. 地理学报, 54(1): 10-20
[29]  唐玉虎,戴霜,黄永波,等. 2008. 兰州—民和盆地河口群沉积相和岩石磁化率:祁连山白垩纪隆升的记录[J]. 地学前缘, 15(2): 261-271
[30]  王成善,胡修绵. 2005. 白垩纪世界与大洋红层[J]. 地学前缘, 12(2): 11-21
[31]  许志琴,杨经绥,李海兵,等. 2011b. 印度—亚洲碰撞大地构造[J]. 地质学报, 85(1): 1-33
[32]  杨经绥,许志琴,张建新,等. 2009. 中国主要高压—超高压变质带的大地构造背景及俯冲/折返机制的探讨[J]. 岩石学报, 25(7): 1529-1560
[33]  杨雨. 1997. 甘肃省岩石地层[M]. 湖北武汉:中国地质大学出版社,1-314
[34]  张二朋,顾其昌,郑文林. 1998. 西北区区域地层[M]. 湖北武汉:中国地质大学出版社,1-221
[35]  Arnott R W C,Zaitlin B A,Potocki D J. 2002. Stratigraphic response to sedimentation in a netaccommodationlimited setting,Lower Cretaceous Basal Quartz,southcentral Alberta[J]. Bulletin of Canadian Petroleum Geology, 50(1): 92-104
[36]  Blair T C,Mcpherson J G. 1994. Alluvialfans and their natural distinction from rivers based on morphology,hydraulic processes,sedimentary processes,and facies assemblages[J]. Journal of Sedimentary Research, 64: 450-489
[37]  Bridge J S. 2006. Fluvial facies models:Recent developments[A]. In:Posamentier H W,Walker R G(eds). Facies Models Revisted[M]. SEPM:Society for Sedimentary Geology,85-170
[38]  Catuneanu O. 2006. Principles of Sequence Stratigraphy[M]. Amsterdam:Elsevier,1-375
[39]  Jinnah Z A,Roberts E M. 2011. Facies associations,paleoenvironment,and baselevel changes in the Upper Cretaceous Wahweap Formation,Utah,U.S.A.[J]. Journal of Sedimentary Research, 81: 266-283
[40]  Leleu S,Hartley A,Williams B P J. 2009. Largescale alluvial architecture and correlation in a Triassic pebbly braided river system,lower Wolfville Formation(Fundy Basin,Nova Scotia,Canada)[J]. Journal of Sedimentary Research, 79: 265-286
[41]  Loope D B,Mason J A,Dingus L. 1999. Lethal sandslides from eolian dunes[J]. Journal of Geology, 107: 707-713
[42]  Marshall J R,Bull P A,Morgan R M. 2012. Energy regimes for aeolian sand grain surface textures[J]. Sedimentary Geology, 253-254: 17-24
[43]  Mei M X,Yu B S,Jin W G. 2004. Sequence stratigraphy of the desert system: A Case study of the Lower Cretaceous in the Kuqa Basin in Xinjiang,northwestern China[J]. Acta Geologica Sinica(English Edition), 78(3): 744-755
[44]  Mountney N P. 2006. Eolian Facies Models[A]. In:Posamentier H W,Walker R G(eds). Facies Models Revisted[M]. Tulsa:SEPM Special Publication 84,19-84
[45]  Nichols G. 2009. Aeolian Environments[A]. In:Nichols G(ed). Sedimentology and Stratigraphy[M]. Chichester of UK:WileyBlackwell,114-128
[46]  Olsen T,Steel R,Hgseth K, et al. 1995. Sequential architecture in a fluvial succession:Sequence stratigraphy in the Upper Cretaceous Mesaverde Group,Price Canyon,Utah[J]. Journal of Sedimentary Research, B65: 265-280
[47]  Plint A,McCarthy P,Faccini U. 2001. Nonmarine sequence stratigraphy:Updip expression of sequence boundaries and systems tracts in a highresolution framework,Cenomanian Dunvegan Formation,Alberta foreland basin,Canada[J]. AAPG Bulletin, 85: 1967-2001
[48]  Sellwood B W,Valdes P J. 2006. Mesozoic climates:General circulation models and the rock record[J]. Sedimentary Geology, 190: 269-287
[49]  Shanley K,McCabe P. 1994. Perspective on the sequence stratigraphy of continental strata[J]. AAPG Bulletin, 78: 544-568
[50]  Simpson E L,HilbertWolf H L,Simpson W S, et al. 2008. The interaction of aeolian and fluvial processes during deposition of the Upper Cretaceous capping sandstone member,Wahweap Formation,Kaiparowits Basin,Utah,U.S.A.[J]. Palaeogeography,Palaeoclimatology,Palaeoecology, 270: 19-28
[51]  Skelton P W. 2003. The Cretaceous World[M]. London:Cambridge University Press,1-350.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133