冀北尚义—隆化区域断裂形成与演化历史探讨

doi:10.19388/j.zgdzdc.2020.05.10

Abstract
Figure/Table
References
Related Citation (9)

Download: PDF (4990 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract Shangyi-Longhua regional fault was EW distributed near northern Hebei Province, which was first active in the Late Neoarchean (Late Fuping) and still active in the Holocene and even today. Therefore, exploring its formation and evolutionary history is of great significance to study its geological structure, mineral distribution and the influence of Neotectonic movement on human beings in northern Hebei Province. The regional faults in Shangyi-Longhua are strong complex deformation zones through the census of the tectonic rocks and all kinds of directional structures in the fault zone. The ductile deformation and brittle deformation are alternating with characters of chronicity, multiphase activity, propensity and nature variation. Shangyi-Longhua regional fault is one of the important dividing lines of tectonic units of different levels in different periods in northern Hebei Province, which plays an important role in controlling the development and evolution of geological history on both sides. The authors redefined the structure superposition transformation relation and the development period, according to the superimposed relationship of the sturcture, the corresponding relationship between metamorphic degree of mylonites and the regional metamorphism, and the corresponding relationship between the movement model reflected by the shear-pointed fabric and the principal stress of the regional tectonic movement. Combined with the metamorphic mineral age of the predecessor tectonites, the authors divided the fault structure into two construction phases and nine tectonic active periods.

Key words： northern Hebei Province Shangyi-Longhua regional fault superposition sturcture evolutionary history

Received: 02 February 2019

P542.3

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	MA Chao
	WANG Jingui
	ZHANG Xinquan
	ZHANG Zixuan
	LI Dian
	ZHANG Xinzheng
	XU Fan

Cite this article:

MA Chao,WANG Jingui,ZHANG Xinquan, et al. Discussion on the formation and evolutionary history of Shangyi-Longhua regional fault in northern Hebei Province[J]. , 2020, 7(5): 88-94.

URL:

http://journal25.magtechjournal.com/Jwk_dzdc/EN/10.19388/j.zgdzdc.2020.05.10 OR http://journal25.magtechjournal.com/Jwk_dzdc/EN/Y2020/V7/I5/88

[1] 河北省地质矿产局.河北省北京市天津市区域地质志[M].北京:地质出版社,1989:566-571.
[2] 程裕淇. 中国区域地质概论[M].北京:地质出版社,1994:145-152.
[3] 胡玲,宋鸿林.“内蒙地轴”南缘断裂带的活动时代及结构分析[J].中国地质,2002,29(4):369-373.
[4] 洪作民. 关于内蒙地轴的东延问题[J].中国区域地质,1988(2):76-80,70.
[5] 王桂梁,刘桂建,邹海,等.华北地台北缘中生代盆-山的耦合转移及其动力学分析[J].煤田地质与勘探,1999,27(6):14-17.
[6] 叶俊林,朱志澄,向树元,等.内蒙地轴南缘盖层中逆冲断层的样式及形成机制[J].地球科学:武汉地质学院学报,1987,12(5):519-527.
[7] 戴凛. 燕山北部尚义—赤城断裂带糜棱岩显微构造特征及其地质意义[D].北京:中国地质大学(北京),2007.
[8] 贾建称. 冀北丰宁—隆化深断裂带的基本特征和演化历史[J].河北地质学院学报,1995,18(4):334-340.
[9] 朱云海,温长顺,叶德隆,等.西赛酸性杂岩体的岩石学和岩石化学特征及其时代讨论[J].现代地质,1996,10(1):36-43.
[10] 胡玲,宋鸿林,颜丹平,等.尚义—赤城断裂带中糜棱岩⁴⁰Ar/³⁹Ar年龄记录及地质意义[J].中国科学(D辑),2002,32(11):908-913.
[11] 杨进辉,吴福元,邵济安,等.冀北张—宣地区后城组、张家口组火山岩锆石U-Pb年龄和Hf同位素[J].地球科学:中国地质大学学报,2006,31(1):71-80.
[12] 张拴宏,赵越,宋彪,等.冀北隆化早前寒武纪高级变质区内的晚古生代片麻状花岗闪长岩——锆石SHRIMP U-Pb年龄及其构造意义[J].岩石学报,2004,20(3):621-626.
[13] 王国灿,谭应佳,王方正.冀北崇礼—赤城大断裂的多相逆冲——兼论内蒙地轴隆升的构造制约因素[J].地球科学:中国地质大学学报,1992,17(6):621-630.
[14] 马军,王仁民.宣化—赤城高压麻粒岩带中蓝晶石-正条纹长石组合的发现及地质意义[J].岩石学报,1995,11(3):273-278.
[15] 张宗清,沈其韩,耿元生,等.赤城伙房村和崇礼上新营变质岩的地球化学特征、年龄及其区域地壳形成时间[J].岩石学报,1996,12(2):315-328.
[16] 刘敦一,耿元生,宋彪.冀西北地区晚太古代大陆地壳的增生和再造——同位素年代学证据[J].地球学报,1997,18(3):226-232.
[17] 赵越. 燕山地区中生代造山运动及构造演化[J].地质论评,1990,36(1):1-13.
[18] 张炯飞,祝洪臣.关于蓟县型中、上元古界沉积环境及内蒙地轴的性质[J].吉林地质,2000,19(4):11-16.
[19] 吴顺发,周治新.冀北赤城—尚义地区航磁数据处理及其地质意义解析[J].黄金地质,1995,1(3):70-75.
[20] 李忠权,刘顺.构造地质学[M].3版.北京:地质出版社,2010:1-22.
[21] 张拴宏. 燕山构造带内蒙古隆起东段晚古生代—早中生代构造岩浆活动及其地质意义[D].北京:中国地质科学院,2004.
[22] 李龙,孙恺孙,胡玲,等.尚义—赤城断裂带西段韧性变形研究[J].地球科学:中国地质大学学报,1995,20(2):33-37.
[23] 牛树银,孙爱群,张建珍,等.华北地台北缘中段构造演化及成矿控矿作用[J].河北地质学院学报,1996,19(3/4):236-246.
[24] 张家声,索书田.华北北部结晶基底中的大型韧性剪切带[J].中国区域地质,1988(4):1-8.
[25] 宋官祥. 一个与碱性杂岩体有关的金矿床——冀北东坪金矿[J].地质与勘探,1991,27(8):1-8.
[26] 刘少峰,张金芳,李忠,等.燕山承德地区晚侏罗世盆地充填记录及对盆缘构造作用的指示[J].地学前缘,2004,11(3):245-254.
[27] 河北省地矿局第三地质大队.下两间房幅、崇礼幅、镇宁堡幅1:5万区域地质调查报告[R].廊坊:河北省地质矿产局区域地质调查大队,1989.
[28] 徐鹏彪,张德生,刘永顺,等.丰宁幅、南关幅、化吉营幅1:5万区域地质调查报告[R].廊坊:河北省区域地质矿产调查研究所,1997.
[29] 胡学文,刘恩华,张江满,等.冀北红旗营子群时代归属及成矿性研究报告[R].廊坊:河北省地质矿产局区域地质调查大队,1989.
[30] 高劢. 燕山地区的太古代绿岩带[M]//张锲.中国改革经纬录.北京:经济日报出版社,1996.
[31] 张春华. 河北早前寒武纪变质作用[M].北京:地质出版社,1990:1-34.
[32] 谭应佳,王国灿,李舜贤.冀北平泉—承德一带太古宙地质及金矿找矿方向[M].武汉:中国地质大学出版社,1991.
[33] Spear F S.梅华林,甘晓春,王惠初,译.确定变质作用P-T-t轨迹的岩石学方法[J].国外前寒武纪地质,1990(3):4-68.
[34] 吴珍汉. 燕山北部崇礼—隆化—阜新构造带形变特征及其控矿作用[J].地质力学学报,1997,3(2):73-81.
[35] 李红阳,张建珍.崇礼—赤城含金剪切带与碱性杂岩体成矿地质特征[J].黄金科学技术,1994,2(2):17-21.
[36] 叶俊林,向树元.河北赤城岩浆岩区逆冲推覆构造特征及其形成机制[J].地球科学:中国地质大学学报,1989,14(1):95-100.
[37] 胡学文,张振利,张永胜,等.石人沟幅(K-50-103-C)、波罗诺幅(K-50-103-D)和红旗幅(K-50-104-C)1:5万区域地质调查报告[R].廊坊:河北省地质矿产局区域地质调查大队,1988.
[38] 陈海燕,张运强,刘蓓蓓,等.冀北承德盆地杏石口组沉积特征及时代讨论[J].中国地质调查,2015,2(8):31-34.
[39] 郝连成,王卫国,胡延斌,等.冀西北怀安地区基底变质岩系构造变形序列研究[J].中国地质调查,2018,5(4):57-66.