Tectono-Thermal Events and Chronological Framework in Zoige and Its Periphery
-
摘要: 通过对川陕甘矿产资源“金三角”地区若尔盖及其周缘沉积建造特征、构造-热事件放射性年代学测试以及磷灰石裂变径迹热年代学测试等综合研究表明，若尔盖地区自印支末期以来，共发生了7次构造-热事件：(1)卡尼末-诺利初期构造-热事件(D1)；(2)早侏罗世(200~180 Ma)构造-热事件(D2)；(3)晚侏罗-早白垩世(160~140 Ma)构造-热事件(D3)；(4)早白垩世(130~110 Ma)构造-热事件(D4)；(5)古新世(70~60 Ma)构造-热事件(D5)；(6)50~40 Ma构造-热事件(D6)；(7)20 Ma左右构造-热事件(D7).其中D1期构造-热事件为若尔盖地区主褶皱造山构造运动，基本奠定若尔盖及其周缘地区区域构造格架；D2、D4为区域关键构造变革期，导致构造-热体制(压性与张性)的关键转换，对区域成矿具有重要意义；最晚期事件(D7期)为青藏高原东北缘高原地貌定型期.Abstract: Based on analysis of the sedimentary features, fission track data, ESR dating and Ar-Ar dating, we argue that there are seven tectono-thermal events in Zoige and its periphery from the Late Triassic. The first tectono-thermal events (D1) took place at the end of the Carnian to the beginning of the Norian stage to form the tectonic framework of Zoige area; the second (D2) and the fourth (D4) tectono-thermal events took place at the early of Jurassic (200－180 Ma) and 130-110 Ma, respectively. They are the key change events in tectonic framework at each time. The seventh (D7) took place at the early of Miocene (~20 Ma), as the most important tectonic event to form the Tibet Plateau. The other three events (D3, D5, D6) took place at 160－140 Ma, 70－60 Ma, 50－40 Ma, respectively.
-
Key words:
- aptatite fission track /
- ESR dating /
- geochronology /
- tectono-thermal events /
- Zoige /
- eastern margin of Tibet
-
图 2 若尔盖地区晚三叠世复理石沉积岩相(古地理)分布
a.卡尼晚期；b.卡尼晚期-诺利早期
Fig. 2. Lithofacies palaeogeography of Late Triassic in in Zoige area
图 3 西秦岭若尔盖及周缘地区放射性测年值统计直方图
参考数据来源：郑明华等，1994；杨俊龙和余必胜，1997；王平安等，1998；邵世才和汪东波，2001；张晓军等，2002；齐金忠等，2003
Fig. 3. Histogram of radiometric ages of Zoige and its periphery in West Qinling
图 4 若尔盖-唐克地区磷灰石裂变径迹反演抬升冷却事件(其中样品TH1、PW1据刘春平，2006)
Fig. 4. Cooling histories and their cooling events from AFT data in Zoige
表 1 若尔盖及周缘地区火成岩同位素测年结果
Table 1. Isotopic dating of igneous rock in Zoige and its periphery
时代 原始样号 采样样点及岩样 年龄(Ma) 补充说明 E 77-R-902 拉尔玛金矿、铀钼型矿石 14~21 U-Pb测年 R-512-34 拉尔玛金矿、铀钼型矿石 22~30 C-112 拉尔玛金矿、铀钼型矿石 24~33 IP-53 东北寨金矿、碳质板岩 41 H-B7 东北寨金矿、若蚀变辉绿玢岩 47 K2 包络错米闪长岩 燕云乡N32°32′，E103°14.16′ 67 年茶铺 斜长花岗斑岩 89.0 K-Ar测 89094 腊子口茶铺、斜长花岗斑岩 102.3±8.2 老虎沟口脉岩 黑河乡N30°34′20″，E104°04′30″ 104±16 Rb-Sr测年 隆雷郎闪长岩 卡隆乡N32°46′，E103°07′ 106 K1 羊拱海花岗岩 黑水县N32°10.37′，E102°37.58′ 110.8 K-Ar测年 达盖寨花岗岩 扎窝乡N32°18′，E103°05.12′ 112 财GS1-5 财宝山、流纹英安岩 112±27 Rb-Sr测年 剑科闪长岩 毛尔盖乡N32°32.33′，E103°02.03′ 115 K-Ar测年 CM48-62 东北寨金矿、薄层泥灰岩 115 U-Pb测年 润德闪长岩 泽盖乡N32°14′，E102°55.59′ 123.2 K-Ar测年 年保也则花岗岩 久治县N32°59′，E101°11.15′ 125.6±3 J3 TC51 降扎、花岗斑岩 151.3±2.0 TC52 降扎、花岗斑岩 156.0±2.0 紫柏杉花岗岩 虎牙乡N32°35.37′，E103°05.57′ 164 D5996TW1 财宝山、英安岩 173.21±4.37 J1-2 崇TW1 崇尔、斜长花岗斑岩 183.2 财TW1-5 财宝山、英安岩 183.2 K-Ar测年 89096 邛莫、次安山岩 183.2±6.6 D6115TW1 财宝山、玄武岩 185.22±4.15 89097 邛莫、次安山岩 186.3±6.7 2842DL 萨木擦库合、闪斜煌斑岩 187.8 纳隆柯闪长岩 红星乡N24°01′00″，E102°46′30″ 189.28 玛洼闪长岩 包坐N33°37.17′，E103°19.67′ 190.7±0.6 U-Pb测年 D5784TW1 财宝山、黑云母 193.74±4.46 K-Ar测年 2984DL 八甘卡、闪长玢岩 195.6±3 T3 贡TW4 贡巴、安山岩 204.8 玄浦沟花岗岩 塔藏乡N32°20′00″，E103°53′30″ 204 U-Pb测年 贡TW16 贡巴、安山岩 206.3 K-Ar测年 参考数据来源：四川省地矿局川西北地质队，1992；杨俊龙和余必胜，1997；采用国际地层年代表，2004. 
下载: 导出CSV
表 2 若尔盖及周边地区电子自旋共振(ESR)测年结果
Table 2. Electron Spin Resonance (ESR) in Zoige and its periphery
时代 样品编号 GPS地点 采样描述 顺磁浓度(15Sp/g) 铀当量(μg/g) 年龄(Ma) E s-7-13-2 N32°53.803′
E103°30.294′川主寺北西郎川公路晚三叠世杂谷脑组石英脉 0.235 1.10 36.0±3.5 s-5-30-1 白依沟 志留系硅质岩石英 0.291 0.67 47.8±5.0 S-6-27-1 N32°36.888′
E101°33.537′安羌乡东5 km处晚三叠世新都桥组石英脉体 0.080 1.25 47.9±5.0 S-7-15-3 N32°20.281′
E103°34.531′马拉墩乡东部晚三叠世新都桥组节理石英脉 0.490 1.06 59.0±6.0 K 06-6-3-1 N32°12.499′
E102°33.473′黑水断裂脆性破裂伴生石英 0.110 1.08 69.8±7.0 06-6-3-2 N32°12.661′
E102°37.437 ′黑水断裂千枚岩左旋石英脉体 0.157 0.57 93.4±9.0 S-7-15-1 N32°35.400′
E103°36.615′雄山村晚三叠世新都桥组节理石英 0.808 0.67 95.6±9.6 R31 N33°28′7.6″
E102°39′16.9″晚三叠世新都桥组粉砂岩顺层条带状石英脉 0.700 1.12 110.5±11.0 NARU组 N35°04.145′
E102°54.464′合作北晚三叠世杂谷脑组切层石英脉体 0.080 1.30 122.1±13.0 S-7-13-1 N32°53.803′
E103°30.294′川主寺北西郎川公路晚三叠世杂谷脑组石英脉 0.270 1.26 127.7±13.0 R15 N33°39′8.3″
E103°20′17.3″巴西电站西晚三叠世杂谷脑组石英脉 0.149 2.56 128.6±13.0 J R35 N33°28′32.8″
E102°39′29′晚三叠世新都桥组砂岩布丁中石英脉 0.808 0.65 143.2±14.0 R17 N33°38′35.1″
E103°20′17.1″晚三叠世侏倭组顺层破碎带石英脉体 0.760 0.54 146.3±14.0 R28 R17W采石场 晚三叠世侏倭组中薄层砂岩层层内石英脉 0.730 1.10 148.6±15.0 R25 R17W采石场 晚三叠世侏倭组破碎带内砂岩中石英脉 0.110 1.08 157.5±16.0 GPS64 N34°28.350′
E104°04.695′岷县北东5 km处顺层节理破裂缝石英脉 0.327 1.60 160.7±16.0 GPS64 N34°28.350′
E104°04.695′岷县北东5 km处切层节理破裂缝石英脉 0.361 0.93 167.3±17.0
下载: 导出CSV
表 3 若尔盖地区样品磷灰石裂变径迹分析结果
Table 3. The fission track analysis data of apatite in Zoige
样号 GPS点 地层 岩性 高程 颗粒数n ρs (105 cm-2)(Ns) ρi (105 cm-2)(Ni) P(χ2)% 中值年龄(Ma)(±1σ) L(μm)(N) HF1
(S210)N33°24′53.2″
E102°33′36.7″T3zh 砂岩 3 578 m 26 1.714
(265)11.372
(1 758)99.5 50±4 13.1±1.8
(92)HF2
(S213)N33°25′35.6″
E102°34′48.8″T3zh 砂岩 3 510 m 25 1.731
(407)8.427
(1 981)68.7 68±5 12.7±1.9
(106)HF3
(S215)N33°27′34.0″
E102°39′00.5″T3zh 砂岩 3 480 m 22 2.446
(334)12.076
(1 649)98.4 67±5 12.5±1.8
(106)HF4
(S221)N33°28′42.3″
E102°39′36.6″T3x 砂岩 3 506 m 21 1.785
(399)9.629
(2 153)82.0 61±4 12.2±1.8
(100)HF5
(S232)N33°29′25.9″
E102°40′11.9″T3zh 砂岩 3 482 m 23 1.448
(272)7.803
(1 466)45.8 61±5 13.4±1.5
(109)注：n=颗粒数；ρs=自发径迹密度；Ns=自发径迹条数；ρi=诱发径迹密度；Ni=诱发径迹条数；P(χ2)=检验概率；中值年龄±σ=径迹年龄±标准差；L=径迹长度；N=封闭径迹条数.样品由中国科学院高能物理所测试.
下载: 导出CSV
表 4 若尔盖地区构造-热事件年代学框架
Table 4. Tectono-thermal events and Chronological Frame in Ruoergai area
构造期 构造-热事件 主要证据 代号 印支末期 卡尼末期-诺利初期 1.沉积建造；2.区域低温动热变质作用；3.U-Pb测年；4.K-Ar测年 D1 早侏罗世(200~180 Ma) 1.K-Ar测年；2.U-Pb测年；3.沉积建造 D2 燕山期 晚侏罗-早白垩世(160~140 Ma) 1.K-Ar测年；2.U-Pb测年；3.ESR测年 D3 早白垩世(130~120 Ma) 1.ESR测年；2.K-Ar测年；3.Rb-Sr测年；4.磷灰石裂变径迹年龄；5.沉积建造 D4 古新世(70~60 Ma左右) 1.ESR测年；2.K-Ar测年；3.磷灰石裂变径迹年龄；4.区域地质资料 D5 喜马拉雅期 50~40 Ma 1.ESR测年；2.U-Pb测年；3.磷灰石裂变径迹年龄；4.岩浆作用 D6 20 Ma左右 1.磷灰石裂变径迹年龄；2.U-Th-Pb测年；3.岩浆作用；4.区域地质资料 D7
下载: 导出CSV
-
[1] Chen, X.H., Chen, Z.L., Han, S.Q., et al., 2012. Geothermochronology of Mo-W Deposits in Balkhash Metallogenic Belt, Kazakhstan, Central Asia. Earth Science—Journal of China University of Geosiciences, 37(5): 878-893 (in Chinese with English abstract). [2] Chen, Y., Liu, S.G., Li Z.W., et al., 2011. LA-ICP-MS Detrital Zircon U-Pb Geochronolgy Approaches to the Sediment Provenance of the Western Sichuan Foreland Basin and Limited Uplift of the Longmen Mountains during the Early Stage of Late Triassic. Geotectonic et Metallogenia, 35(2): 315-323 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DGYK201102018.htm [3] Chen, Y.J., Zhang, J., Zhang, F.X., et al., 2004. Carlin and Carlin-Like Gold Deposits in Western Qinling Mountains and Their Metallogenic Time, Tectonic Setting and Model. Geological Review, 50(2): 134-152 (in Chinese with Enligsh abstract). http://www.researchgate.net/publication/274565354_Carlin_and_Carlin-like_Gold_Deposits_in_Western_Qinling_Mountains_and_Their_Metallogenic_Time_Tectonic_Setting_and_Model [4] Chen, W.J., Li, Q., 1999. MDD Model and Rapid Cooling Events. Earth Science Frontiers, 6(4): 371-377 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY199904030.htm [5] Chen, Z.L., Liu, Y.P., Tang, W.Q., et al., 2006. Recent Deformation and Displacement of Continental Lithosphere in the Northeastern Margin of Qinhai-Tibet Plateau. Geological Bulletin of China, 25(1-2): 20-28 (in Chinese with English abstract). http://www.researchgate.net/publication/296019010_Recent_deformation_and_displacement_of_continental_lithosphere_in_the_northeastern_margin_of_Qinghai_-_Tibet_Plateau_Geological_Bulletin_of_China [6] Dai, W.J., Dang, Y.Y., Liu, S.X., et al., 2001. Feature and Tectonic Setting of Volvanic Rock of Median Jurassic System in Zizihe Area, Xiahe County. Acta Geologica Gansu, 10(2): 23-28 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GSDZ200102002.htm [7] Deng, B., Liu, S.G., Jansa, L., et al., 2012a. Sedimentary Record of Late Triassic Transpressional Tectonics of the Longmenshan Thrust Belt, SW China. Journal of Asian Earth Sciences, 48(2): 43-55. doi: 10.1016/j.jseaes.2011.12.019 [8] Deng, B., Liu, S.G., Li, Z.W., et al., 2012b. Late Cretaceous Tectonic Change of the Eastern Margin of the Tibetan Plateau-Results from Multisystem Thermochronology. Journal Geological Society of India, 80(2): 241-254. doi: 10.1007/s12594-012-0134-8 [9] Deng, B., Liu, S.G., Li, Z.W., et al., 2008. A Comparative Study of the Late Mesozoic Uplifting in the Eastern Margin of Qinghai-Tibet Plateau and Sichuan Basin. Journal of Chengdu University of Technology (Science & Technology Edition), 35(4): 477-486 (in Chinese with English abstract). http://www.researchgate.net/publication/286885476_A_comparative_study_of_the_late_Mesozoic_uplifting_in_the_eastern_margin_of_Qinghai-Tibet_plateau_and_Sichuan_basin_China [10] Deng, B., Liu, S.G., Li, Z.W., et al., 2009. Uplifting Characteristics in Eastern Margin Area of Tibetan Plateau: Evidence from Low-Temperature Thermochronology. Quaternary Sciences, 29(3): 594-606 (in Chinese with English abstract). [11] Enkelmann, E., Ratschbacher, L., Jonckheere, R., et al., 2006. Cenozoic Exhumation and Deformation of Northeastern Tibet and the Qinling: Is Tibetan Lower Crustal Flow Diverging around the Sichuan Basin?GSA Bulletin, 118(5-6): 651-671. doi: 10.1130/B25805.1 [12] Gao, R., Ma, Y.S., Liu, Q.S., et al., 2006. Structure of the Lower Crust Beneath the Songpan Block and West Qinling Orogen and Their Relation as Revealed by Deep Seismic Reflection Profiling. Geological Bulletin of China, 25(12): 411-418 (in Chinese with English abstract). http://www.researchgate.net/publication/283809135_Structure_of_the_lower_crust_beneath_the_Songpan_block_and_West_Qinling_orogen_and_their_relation_as_revealed_by_deep_seismic_reflection_profiling [13] Grun, R., 1989. ESR Dating for the Early Earth. Nature, 338: 543-544. doi: 10.1038/338543a0 [14] Hu, J.M., Meng, Q.R., Shi, Y.R., et al., 2005. SHRIMP U-Pb Dating of Zircons from Granitoid Bodies in the Songpan-Ganzi Terrane and Its Implication. Acta Petrologica Sinica, 21(3): 867-880 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200503027.htm [15] Li, Y., Zeng, Y.F., 1995. Stratigraphic Signatures to Thrusting of the Longmen Mountains Thrust Belt. Journal of Chengdu Institute of Technology, 22(2): 1-10 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG502.000.htm [16] Liang, X.Z., Gao, J.C., 1999. Study on the α-Quartz Dating of Fault-Related Ore Mineralization. Journal of Mineralogy and Petrology, 19(2): 69-71 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWYS902.014.htm [17] Liu, C.P., 2006. The Tectonic Evolution and the Basic Petroleum Condition in Songpan-Aba Basin(Disseration). China University of Geosciences, Beijing (in Chinese with English abstract). [18] Liu, J.J., Feng, C.X., Liu, J.M., et al., 2004 Reidentification of the Ore-Hosted Strata Age and Metallogenic Age of the Stratabound Au-Se Deposits, the Western Qinling Mountains. Earth Science Frontiers, 11(2): 435-443 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200402018.htm [19] Liu, H., Wang, G.C., Cao, S.Z., et al., 2012. Discovery of Nanhuaian Biomodal Volcanics in Northern Altyn Tagh and Its Tectonic Significance. Earth Science—Journal of China University of Geosciences, 37(5): 917-929 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201205007.htm [20] Liu, S.G., Li, Z.W., Cao, J.X., et al., 2009.4-D Textural and Structural Characteristic of Longmen Intracontinental Composite Orogenic Belt, Southwest China. Chinese Journal of Geology, 44(4): 1151-1180 (in Chinese with English abstract). http://www.researchgate.net/publication/279543050_D_textural_and_structural_characteristics_of_Longmen_intracontinental_composite_orogenic_belt_southwest_China._Chinese_Jour._Geol_v.44_pp.1151-1180 [21] Liu, S.G., Li, Z.W., Sun, W., et al., 2011. Basic Geolgoical Features of Superimposed Basin and Hydrocarbon Accumulation in Sichuan Basin, China. Chinese Journal of Geology, 46(1): 233-257 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKX201101020.htm [22] Liu, S.G., Luo, Z.L., Dai, S.L., et al., 1996. The Uplift of the Longmenshan Thrust Belt and Subsidence of the West Sichuan Foreland Basin. Acta Geological Sinica-English Edition, 9(1): 16-26. doi: 10.1111/j.1755-6724.1996.mp9001002.x [23] Liu, S.G., Zhao, X.K., Luo, Z.L., et al., 2001. Study on the Tectonic Events in the System of the Longmen Mountain-West Sichuan Foreland Basin, China. Journal of Chengdu University of Technology (Science & Technology Edition), 28(3): 221-231 (in Chinese with English abstract). http://www.researchgate.net/publication/279545731_Study_on_the_tectonic_events_in_the_system_of_the_Longmen_Mountain-West_Sichuan_Foreland_Basin_China [24] Luo, M., Zhu, W.B., Zhang, B.H., et al., 2012. Mesozoic-Cenozoic Tectonic Evolution of the Kuqa Basin: Evidence from Apatite Fission-Track Data. Earth Science—Journal of China University of Geosciences, 37(5): 893-903 (in Chinese with English abstract). [25] Ma, Y.S., Shi, W., Zhang, Y.Q., et al., 2005. Characteristics of the Activity of the Maqu Segment of the East Kunlun Active Fault Belt and Its Eastward Extension. Geological Bulletin of China, 24(1): 30-35(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200501005.htm [26] Qi, J.Z., Yuan, S.S., Li, L., et al., 2003. Geological Features and Ore-Controlling Factors of the Yanshan Superlarge Gold Deposit, Gansu Province, China. Geological Review, 49(1): 85-92 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200301012.htm [27] Roger, F., Malavieille, J., Leloup, P.H., et al., 2004. Timing of Granite Emplacement and Cooling in the Songpan-Ganze Fold Belt (Eastern Tibetan Plateau) with Tectonic Implications. Journal of Asian Earth Sciences, 22(5): 465-481. doi: 10.1016/S1367-9120(03)00089-0 [28] Shao, S.C., Wang, D.B., 2001. Ar-Ar Dating of Three Typical Gold Deposits and Its Geological Significance in the Southern Qinling Region. Acta Geologica Sinica, 75(1): 106-110 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/ http://search.cnki.net/down/default.aspx?filename=DZXE200101016&dbcode=CJFD&year=2001&dflag=pdfdown [29] Sichuan Bureau of Geology and Mineral Resoures, 1991. Regional Geology of Sichuan Province. Geological Publishing House, Beijing (in Chinese). [30] Sichuan Northwest Geological Team, 1992.1∶50 000 Regional Geology of Gongba, Zhagana Area. Geological Publishing House, Beijing (in Chinese). [31] Wang, P.A., Chen, Y.C., Pei, R.F., 1998. Regional Metallogenic Series and Tectono-Metallogenic Cycles and Evolution of the Qinling Orogen. Geological Publishing House, Beijing (in Chinese). [32] Weislogel, A.L., Graham, S.A., Chang, E.Z., et al., 2006. Detrital Zircon Provenance of the Late Triassic Songpan-Ganzi Complex: Sedimentary Record of Collision of the North and South China Blocks. Geology, 34(2): 97-100. doi: 10.1130/G21929.1 [33] Xu, Z.Q., Hou, L.W., Wang, Z.X., et al., 1992. Orogenic Processes of the Songpan-Garze Orogenic Belt of China. Geological Publishing House, Beijing (in Chinese). [34] Yang, J.L., Yu, B.S., 1997. U-Th-Pb Geochronology and Lead Isotope Geochemistry of the La'erma Carlin Type Gold Deposit in West Qinling Mountain. Geology and Mineral Resources of South China, 4: 39-49 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNKC199704005.htm [35] Yang, K.G., Liang, X.Z., Xie, J.L., et al., 2006. EAR Dating, the Principle and Application of a Method to Determine Active Ages of Brittle Faults. Advances in Earth Science, 21(4): 430-435 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXJZ200604013.htm [36] Yin, A., Nie, S., 1993. An Indentation Model for the North and South China Collision and the Development of Tanlu and Honam Fault Systems, Eastern Asia. Tectonics, 12(4): 801-813. doi: 10.1029/93TC00313 [37] Yin, H.F., Yang, F.Q., Huang, Q.S., et al., 1992. The Triassic of Qinling Mountains and Nieghboring Areas. China University of Geosciences Press, Wuhan(in Chinese). [38] Yu, X.H., Zhao, Z.D., Mo, X.X., et al., 2005. 40Ar-39Ar Dating and Its Implication of Cenozoic Kamafugite in Western Qinling, Gansu. Chinese Science Bulletin, 50(23): 2638-2643 (in Chinese). doi: 10.1360/csb2005-50-23-2638 [39] Zhang, G.W., Guo, A.L., Yao, A.P., 2004. Western Qinling-Songpan Continental Tectonic Nodein China's Continental Tectonics. Earth Science Frontiers, 11(3): 23-32 (In Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dxqy200403004.htm [40] Zhang, K.X., Wang, G.C., Chen, F.N., et al., 2007. Coupling between the Uplift of Qinghai-Tibet Plateau and Distribution of Basin of Paleogene-Neogene. Earth Science—Journal of China University of Geosciences, 32(5): 583-579 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200705002.htm [41] Zhang, H.F., Parrish, R., Zhang, L., et al., 2007. A-Type Granite and Adakitic Magmatism Association in Songpan-Garze Fold Belt, Eastern Tibetan Plateau: Implication for Lithospheric Delamination. Lithos, 97(3-4): 323-335. doi: 10.1016/j.lithos.2007.01.002 [42] Zhang, H.F., Zhang, L., Harris, N., et al., 2006. U-Pb Zircon Ages, Geochemical and Isotopic Compositions of Granitoids in Songpan-Garze Fold Belt, Eastern Tibetan Planteau: Constraints on Petrogenesis and Tectonic Evolution of the Basement. Contib. Mineral. Petrol. , 152(1): 75-88. doi: 10.1007/s00410-006-0095-2 [43] Zhang, Z.L., Zhang, P., Yuan, H.H., 1991. The Geochemical Information of Dynamical Mechamism Forming Longmenshan Mountains. Journal of Chengdu College of Geology, 18(1): 23-32 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG199101005.htm [44] Zhang, X.J., Zhang, J., Jia, Y.S., et al., 2002. Geological and Geochemical Features of the Jinmuda Gold Deposit in Northwestern Sichuan Province. Geology and Prospecting, 38(3): 28-32 (in Chinese with English abstract). http://www.researchgate.net/publication/294696535_Geological_and_geochemical_features_of_the_Jinmuda_gold_deposit_in_northwestern_Sichuan_province [45] Zhao, Y.J., Yuan, C., Zhou, M.F., et al., 2007. Post-Orogenic Extension of Songpan-Ganzi Orogen in Early Jurassic: Constrains from Niuxingou Monzodiorite and Siguniangshan A-Type Granite of Western Sichuan, China. Geochimica, 36(2): 139-152 (in Chinese with English abstract). [46] Zheng, M.H., 1994. Stratabound Gold Deposits of Exhalation Type and Turbidity Type. Sichuan Publishing House of Science & Technology, Chengdu(in Chinese). [47] 陈宣华, 陈正乐, 韩淑琴, 等, 2012. 中亚巴尔喀什成矿带钼-钨矿的地质热年代学. 地球科学——中国地质大学学报, 37(5): 878-893. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201205003.htm [48] 陈杨, 刘树根, 李智武, 等, 2011. 川西前陆盆地晚三叠世早期物源与龙门山的有限隆升——碎屑锆石U-Pb年代学研究. 大地构造与成矿学, 35(2): 315-323. doi: 10.3969/j.issn.1001-1552.2011.02.017 [49] 陈衍景, 张静, 张复新, 等, 2004. 西秦岭地区卡林-类卡林型金矿床及其成矿时间构造背景和模式. 地质论评, 50(2): 134-152. doi: 10.3321/j.issn:0371-5736.2004.02.004 [50] 陈文寄, 李齐, 1999. MDD模式与快速冷却事件. 地学前缘, 6(4): 371-377. doi: 10.3321/j.issn:1005-2321.1999.04.021 [51] 陈智梁, 刘宇平, 唐文清, 等, 2006. 青藏高原东北缘大陆岩石圈现今变形和位移. 地质通报, 25(1-2): 20-28. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2006Z1005.htm [52] 代文军, 党引业, 柳生祥, 等, 2001. 夏河县孜孜合一带中侏罗世火山岩特征及构造环境探讨. 甘肃地质学报, 10(2): 23-28. https://www.cnki.com.cn/Article/CJFDTOTAL-GSDZ200102002.htm [53] 邓宾, 刘树根, 李智武, 等, 2008. 青藏高原东缘及四川盆地晚中生代以来隆升作用对比研究. 成都理工大学学报(自然科学版), 35(4): 477-486. doi: 10.3969/j.issn.1671-9727.2008.04.018 [54] 邓宾, 刘树根, 李智武, 等, 2009. 青藏高原东缘地区隆升作用特征-低温年代学证据. 第四纪研究, 29(3): 594-606. https://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200903019.htm [55] 高锐, 马永生, 李秋生, 等, 2006. 松潘地块若尔盖盆地与西秦岭造山带岩石圈尺度的构造关系——深地震反射剖面探测成果. 地球学报, 25(12): 411-418. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200605004.htm [56] 胡健民, 孟庆任, 石玉若, 等, 2005. 松潘-甘孜地体内花岗岩锆石SHRIMP U-Pb定年及其构造意义. 岩石学报, 21(3): 867-880. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200503027.htm [57] 李勇, 曾允孚, 1995. 龙门山逆冲推覆作用的地层标识. 成都理工学院学报, 22(2): 1-10. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG502.000.htm [58] 梁兴中, 高钧成, 1999. 断裂成矿年龄的α石英ESR研究. 矿物岩石, 19(2) : 69-71. https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS902.014.htm [59] 刘春平, 2006. 松潘-阿坝盆地构造演化与石油地质基本条件(博士学位论文). 北京: 中国地质大学. [60] 刘函, 王国灿, 曹树钊, 等, 2012. 北阿尔金南华纪双峰式火山岩的发现及构造意义. 地球科学——中国地质大学学报, 37(5): 917-929. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201205007.htm [61] 刘树根, 罗志立, 戴苏兰, 1996. 四川前陆盆地的"四川运动"及与油气的关系. 石油与天然气地质, 17(4): 276-281. doi: 10.3321/j.issn:0253-9985.1996.04.004 [62] 刘树根, 赵锡奎, 罗志立, 等, 2001. 龙门山造山带-川西前陆盆地系统构造事件研究. 成都理工学院学报, 28(3): 221-231. doi: 10.3969/j.issn.1671-9727.2001.03.001 [63] 刘树根, 李智武, 曹俊兴, 等, 2009. 龙门山陆内复合造山带的四维结构构造特征. 地质科学, 44(4): 1151-1180. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200904012.htm [64] 刘树根, 李智武, 孙玮, 等, 2011. 四川含油气叠合盆地基本特征. 地质科学, 46(1): 233-257. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX201101020.htm [65] 刘家军, 冯彩霞, 刘建明, 等, 2004. 西秦岭南亚带层控金-硒矿床的赋矿地层年代与成矿时代. 地学前缘, 11(2): 435-443. doi: 10.3321/j.issn:1005-2321.2004.02.013 [66] 罗梦, 朱文斌, 郑碧海, 等, 2012. 库车盆地中新生代构造演化: 磷灰石裂变径迹证据. 地球科学——中国地质大学学报, 37(5): 893-903. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201205004.htm [67] 马寅生, 施炜, 张岳桥, 等, 2005. 东昆仑活动断裂带玛曲段活动特征及其东延. 地质通报, 24(1): 30-35. doi: 10.3969/j.issn.1671-2552.2005.01.005 [68] 齐金忠, 袁士松, 李莉, 等, 2003. 甘肃省文县阳山特大型金矿床地质特征及控矿因素分析. 地质论评, 49(1): 85-92. doi: 10.3321/j.issn:0371-5736.2003.01.013 [69] 邵世才, 汪东波, 2001. 南秦岭3个典型金矿床的Ar-Ar年代学及其地质意义. 地质学报, 75(1): 106-110. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200101016.htm [70] 四川省地矿局川西北地质队, 1992. 贡巴、扎尕那等1∶5万八副联测区调报告. 北京: 地质出版社. [71] 四川省地质矿产局, 1991. 四川省区域地质志. 北京: 地质出版社. [72] 王平安, 陈毓川, 斐荣富, 1998. 西秦岭造山带区域矿床成矿系列、构造-成矿旋回与演化. 北京: 地质出版社. [73] 许志琴, 侯立玮, 王宗秀, 等, 1992. 中国松潘-甘孜造山带的造山过程. 北京: 地质出版社. [74] 杨俊龙, 余必胜, 1997. 西秦岭拉尔玛卡林型金矿床的U-Th-Pb年代学与Pb同位素地球化学研究. 华南地质与矿产, 4: 39-49. https://www.cnki.com.cn/Article/CJFDTOTAL-HNKC199704005.htm [75] 杨坤光, 梁兴中, 谢建磊, 等, 2006. ESR定年: 一种确定脆性断层活动年龄的方法原理与应用. 地球科学进展, 21(4): 430-435. doi: 10.3321/j.issn:1001-8166.2006.04.013 [76] 殷鸿福, 杨逢清, 黄其胜, 等, 1992. 秦岭及邻区三叠系. 武汉: 中国地质大学出版社. [77] 喻学惠, 赵志丹, 莫宣学, 等, 2005. 甘肃西秦岭新生代钾霞橄黄长岩的40Ar/39Ar同位素定年及其地质意义. 科学通报, 50(23): 2638-2643. doi: 10.3321/j.issn:0023-074X.2005.23.013 [78] 张国伟, 郭安林, 姚安平, 2004. 中国大陆构造中的西秦岭—松潘大陆构造结. 地学前缘2004, 11(3): 23-32. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200403004.htm [79] 张克信, 王国灿, 陈奋宁, 等, 2007. 青藏高原古近纪-新近纪隆升与沉积盆地分布耦合. 地球科学, 32(5): 583-579. doi: 10.3321/j.issn:1000-2383.2007.05.001 [80] 张志兰, 张平, 袁海华, 1991. 龙门山形成动力机制的地球化学信息. 成都地质学院学报, 18(1): 23-32. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG199101005.htm [81] 张晓军, 张均, 贾永胜, 等, 2002. 川西北金木达矿床地质地球化学特征研究. 地质与勘探, 38(3): 28-32. doi: 10.3969/j.issn.0495-5331.2002.03.005 [82] 赵永久, 袁超, 周美夫, 等, 2007. 松潘甘孜造山带早侏罗世的后造山伸展: 来自川西牛心沟和四姑娘山岩体的地球化学制约. 地球化学, 36(2): 139-152. doi: 10.3321/j.issn:0379-1726.2007.02.003 [83] 郑明华, 1994. 喷流型与浊流型层控金矿床. 成都: 四川科学技术出版社. -
点击查看大图
图(4) / 表(4)
计量
- 文章访问数: 3228
- HTML全文浏览量: 177
- PDF下载量: 591
- 被引次数: 0
