The spatial and temporal evolution of thermal stress after granite emplacement and its influencing factors

ZHAO Yuda; ZHANG Wengao; LIU Hao; LIU Xiangchong

doi:10.12090/j.issn.1006-6616.2023157

Volume 30 Issue 1

Feb. 2024

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ZHAO Y D，ZHANG W G，LIU H，et al.，2024. The spatial and temporal evolution of thermal stress after granite emplacement and its influencing factors[J]. Journal of Geomechanics，30（1）：38−56 doi: 10.12090/j.issn.1006-6616.2023157

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The spatial and temporal evolution of thermal stress after granite emplacement and its influencing factors

doi: 10.12090/j.issn.1006-6616.2023157

ZHAO Yuda^{1, 2
,},
ZHANG Wengao^{1, 3, 4},
LIU Hao^{1, 5},
LIU Xiangchong^{1, 3, 4
,
,}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
3.
Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China
4.
The Laboratory of Dynamic Diagenesis and Metallogenesis, Institute of Geomechanics, CAGS, Beijing 100081, China
5.
School of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China

Funds: This research is financially supported by the Open Fund of the Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources (Grant No. MREBZ-2023-OF02), the Basic Research Operation Funds of the Chinese Academy of Geological Sciences (Grant No. JKYQN202339), and the Geological Survey Project of the China Geological Survey (Grant No. DD20230344).

More Information

Received: 2023-08-01
Revised: 2023-10-08
Accepted: 2024-01-15

Available Online: 2024-02-09

Published: 2024-02-01

Abstract

Abstract

Objective Granitic magmas are genetically associated with magmatic-hydrothermal deposits and oil and gas reservoirs. The emplacement of granitic magmas into cooler rocks produced thermal anomaly and thermal stress, yet systematic studies on the spatial and temporal evolution of thermal stress still need to be completed. Previous numerical modeling often used rocks' linear thermal expansion coefficient at room temperature, but this parameter is highly temperature-dependent and reaches much higher levels at high temperatures. Therefore, the magnitude of the thermal stress caused by magma emplacement needs to be re-examined. A series of numerical experiments were carried out to investigate how the surrounding rock's lithology (granite or carbonate rocks), Young's modulus, thermal parameters, and the depth of magma emplacement affect the thermal stress generated by the magma in the overlying surrounding rocks. Methods Because the magma cools and eventually reaches thermal equilibrium with the surrounding strata, numerical simulation is one of the common methods to examine the thermal stress after magma emplacement quantitatively. This article used FLAC^3D software to simulate the thermal stress caused by the emplacement of granitic magma into the upper crust. The differential equations we solved include the thermal conduction and linear thermoelasticity equations. The models' thermal field influences the stress field through temperature difference and the linear thermal expansion coefficient. However, changes in the stress field do not affect the thermal field, i.e., one-way coupling between the thermal field and the stress field. Results (1) Heat transfer is quicker on wallrocks with high thermal conductivity, causing a faster change in thermal stress. Compared to the high-thermal-conductivity case, the same thermal stress can be produced on wallrocks with a lower thermal conductivity after a more extended period of magma cooling. (2) The thermal stress produced by the surrounding rock's Young's modulus of 80 GPa is higher than the surrounding rock's Young's modulus of 60 GPa and 40 GPa. (3)The thermal stress simulated in the article is an order of magnitude larger than those generated using the linear coefficient of thermal expansion at room temperature. The thermal stress induced by granite surrounding rocks is nearly 30 MPa higher than that induced by carbonate rocks. (4) The thermal stress decreases with increasing distance from magma, approaching the initial stresses at nearly 2 km. (5) When the emplacement depth is shallow, both initial temperature and initial stress are lower than those in deeper emplacements; The magma room cools faster at shallow depths. Because the initial temperature of magma is the same, shallow emplacements will produce higher thermal stresses on overlying surrounding rocks. Conclusion The modeling results indicate that the thermal conductivity of surrounding rocks influences the change rate of thermal stress through the heat transfer rate. The thermal stress increases with the surrounding rock's Young's modulus. Since the average Young's modulus of granites is greater than that of carbonate rocks, the thermal stress on granite is greater than that on carbonate rocks. Either granites or carbonate rocks at high temperatures have a thermal expansion coefficient about one order of magnitude greater than that at room temperature, resulting in thermal stress of up to 100 MPa. The temperature of the surrounding rock gradually increases after the granite magma emplacement, corresponding to the increasing thermal stress. The thermal stress decreases with increasing distance from magma, exerting no influence on the initial stress of host rocks above 2 km of the granitic magma. When the magma emplacement is shallow, the combination of high thermal stress and low initial stress is more conducive to the formation and expansion of fractures in overlying surrounding rock. Significance The results of numerical simulations reveal that the thermal stresses generated by magma emplacement can affect the stress field 2 km above the magma. These localized and short-lived thermal stresses may fracture the overlying rocks, providing transport channels or ore-bearing spaces for later hydrothermal fluids.
- granite cooling,
- magmatic thermal field,
- numerical modeling,
- thermal stress,
- linear thermal expansion coefficient

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References(122)

References

[1]	ABOOTALEBI P, SIEMENS G, 2018. Thermal properties of engineered barriers for a Canadian deep geological repository[J]. Canadian Geotechnical Journal, 55(6): 759-776. doi: 10.1139/cgj-2017-0150
[2]	AHRENS T J, 1995. Mineral physics & crystallography: a handbook of physical constants[M]. Washington: American Geophysical Union.
[3]	ANNEN C, LATYPOV R, CHISTYAKOVA S, et al. , 2022. Catastrophic growth of totally molten magma chambers in months to years[J]. Science Advances, 8(38): eabq0394. doi: 10.1126/sciadv.abq0394
[4]	ARTEMIEVA I M, THYBO H, JAKOBSEN K, et al. , 2017. Heat production in granitic rocks: Global analysis based on a new data compilation GRANITE2017[J]. Earth-Science Reviews, 172: 1-26. doi: 10.1016/j.earscirev.2017.07.003
[5]	BARBOZA S A, BERGANTZ G W, 1996. Dynamic model of dehydration melting motivated by a natural analogue: applications to the Ivrea–Verbano zone, northern Italy[J]. Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 87(1-2): 23-31. doi: 10.1017/S0263593300006441
[6]	BEA F, 2012. The sources of energy for crustal melting and the geochemistry of heat-producing elements[J]. Lithos, 153: 278-291. doi: 10.1016/j.lithos.2012.01.017
[7]	BERGBAUER S, MARTEL S J, HIERONYMUS C F, 1998. Thermal stress evolution in cooling pluton environments of different geometries[J]. Geophysical Research Letters, 25(5): 707-710. doi: 10.1029/98GL00047
[8]	BERGBAUER S, MARTEL S J, 1999. Formation of joints in cooling plutons[J]. Journal of Structural Geology, 21(7): 821-835. doi: 10.1016/S0191-8141(99)00082-6
[9]	BIOT M A, 1956. Thermoelasticity and irreversible thermodynamics[J]. Journal of Applied Physics, 27(3): 240-253. doi: 10.1063/1.1722351
[10]	BOHRSON W A, SPERA F J, 2001. Energy-constrained open-system magmatic processes II: application of energy-constrained assimilation–fractional crystallization (EC-AFC) model to magmatic systems[J]. Journal of Petrology, 42(5): 1019-1041. doi: 10.1093/petrology/42.5.1019
[11]	CAO H W, 2015. Research on Mesozoic-Cenozoic magmatic evolution and its relation with metallogeny in Tengchong-Lianghe tin ore belt, Western Yunnan[D]. Beijing: China University of Geosciences (Beijing): 1-340. (in Chinese with English abstract)
[12]	CATHLES L M, ERENDI A H J, BARRIE T, 1997. How long can a hydrothermal system be sustained by a single intrusive event? [J]. Economic Geology, 92(7-8): 766-771. doi: 10.2113/gsecongeo.92.7-8.766
[13]	CEN K, TIAN Z X, 2012. Ore-forming system around magma — model of spatial zonation for magmatic rock and deposit set[J]. Geoscience, 26(5): 1051-1057. (in Chinese with English abstract)
[14]	CHANG C, LUO G, 2022. The fracture forming mechanism at the top of the intrusion body in porphyry deposits: the insights from a multi-physical field coupled numerical model[J]. Chinese Journal of Geophysics, 65(8): 3006-3024. (in Chinese with English abstract)
[15]	CHAPPELL B W, WHITE A J R, WILLIAMS I S, et al. , 2004. Low- and high-temperature granites[J]. Transactions of the Royal Society of Edinburgh: Earth Sciences, 95, 125–140.
[16]	CHEN B L, GAO Y, 2022. Study on ore-bearing fracture system of veinlet orebody in Tongchang porphyry copper deposit, Dexing of Jiangxi[J]. Mineral Deposits, 41(6): 1093-1107. (in Chinese with English abstract)
[17]	CHEN Y, WU X D, ZHANG F Q, 1999. Experimental study on thermal cracking of rocks[J]. Chinese Science Bulletin, 44(8): 880-883. (in Chinese) doi: 10.1360/csb1999-44-8-880
[18]	CHEN Y M, XU D P, 2013. FLAC/FLAC 3D fundamentals and engineering examples[M]. 2nd ed. Beijing: China Water & Power Press. (in Chinese)
[19]	COLEMAN D S, GRAY W, GLAZNER A F, 2004. Rethinking the emplacement and evolution of zoned plutons: Geochronologic evidence for incremental assembly of the Tuolumne Intrusive Suite, California[J]. Geology, 32(5): 433-436. doi: 10.1130/G20220.1
[20]	CRUDEN A R, MCCAFFREY K J W, 2001. Growth of plutons by floor subsidence: implications for rates of emplacement, intrusion spacing and melt-extraction mechanisms[J]. Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy, 26(4-5): 303-315. doi: 10.1016/S1464-1895(01)00060-6
[21]	DWIVEDI R D, GOEL R K, PRASAD V V R, et al. , 2008. Thermo-mechanical properties of Indian and other granites[J]. International Journal of Rock Mechanics and MINING SCIENCES, 45(3): 303-315. doi: 10.1016/j.ijrmms.2007.05.008
[22]	DUHAMEL J M C, 1837. Second mémoire sur les phénoménes thermo-mécaniques[J]. J de l’École Polytechnique,15（25）: 1–57.
[23]	ELLIS J F, BLENKINSOP T, 2019. Analogue modelling of fracturing in cooling plutonic bodies[J]. Tectonophysics, 766: 14-19. doi: 10.1016/j.tecto.2019.05.019
[24]	ENGLISH J M, 2012. Thermomechanical origin of regional fracture systems[J]. AAPG Bulletin, 96(9): 1597-1625. doi: 10.1306/01021211018
[25]	ESLAMI M R, HETNARSKI R B, IGNACZAK J, et al. , 2013. Theory of elasticity and thermal stresses: explanations, problems and solutions[M]. Dordrecht: Springer.
[26]	EVANS D J, ROWLEY W J, CHADWICK R A, et al. , 1994. Seismic reflection data and the internal structure of the Lake District batholith, Cumbria, northern England[J]. Proceedings of the Yorkshire Geological Society, 50: 11-24. doi: 10.1144/pygs.50.1.11
[27]	FAN Y L, GAO J W, YU S, et al. , 2023. Prediction and analysis on large deformation of surrounding rocks in the Muzhailing Tunnel of the Weiyuan–Wudu Expressway under high in-situ stress[J]. Journal of Geomechanics, 29(6): 786-800. (in Chinese with English abstract)
[28]	FANG G C, WANG D H, FENG Z X, et al. , 2021. The fan-like distribution of ore veins in the quartz-vein type tungsten deposits in South China and its prospecting significance[J]. Geotectonica et Metallogenia, 45(3): 523-533. (in Chinese with English abstract)
[29]	FOURIER J B J, 2009. The analytical theory of heat[M]. Cambridge: Cambridge University Press: 466.
[30]	FU H F, ZHANG B H, GE J H, et al. , 2019. Thermal diffusivity and thermal conductivity of granitoids at 283-988 K and 0.3-1.5 GPa [J]. American Mineralogist, 104(11): 1533-1545. doi: 10.2138/am-2019-7099
[31]	GERCEK H, 2007. Poisson's ratio values for rocks[J]. International Journal of Rock Mechanics and Mining Sciences, 44(1): 1-13. doi: 10.1016/j.ijrmms.2006.04.011
[32]	GERDES M L, BAUMGARTNER L P, PERSON M, 1998. Convective fluid flow through heterogeneous country rocks during contact metamorphism[J]. Journal of Geophysical Research: Solid Earth, 103(B10): 23983-24003. doi: 10.1029/98JB02049
[33]	GERLA P J, 1988. Stress and fracture evolution in a cooling pluton: An example from the Diamond Joe stock, western Arizona, U. S. A. [J]. Journal of Volcanology and Geothermal Research, 34(3-4): 267-282. doi: 10.1016/0377-0273(88)90038-8
[34]	GHIORSO M S, 1991. Temperatures in and around cooling magma bodies[M]//PERCHUK L L. Progress in metamorphic and magmatic petrology: a memorial volume in Honour of D. S. Korzhinskiy. Cambridge: Cambridge University Press: 387-410.
[35]	GU D S, LI X B, 2003. Science problems and research state of deep mining in metal and nonferrous mines[J]. Mining Research and Development, 23(S1): 1-5. (in Chinese with English abstract)
[36]	Guangdong Nonferrous Metal Geological Exploration Company 932 Team, 1966. How we use the "five-story" law to find, evaluate and explore wolframite quartz vein deposits[J]. Geology and Exploration, (5): 15-19. (in Chinese)
[37]	GUILLOU-FROTTIER L, BUROV E, 2003. The development and fracturing of plutonic apexes: implications for porphyry ore deposits[J]. Earth and Planetary Science Letters, 214(1-2): 341-356. doi: 10.1016/S0012-821X(03)00366-2
[38]	HAN X H, CHU Z H, ZHANG Y Z, 2005. Thermal-induced rock cracking and its significance in engineering[J]. Petroleum Geology & Experiment, 27(1): 98-100. (in Chinese with English abstract)
[39]	HEARD H C, PAGE L, 1982. Elastic moduli, thermal expansion, and inferred permeability of two granites to 350°C and 55 megapascals[J]. Journal of Geophysical Research: Solid Earth, 87(B11): 9340-9348. doi: 10.1029/JB087iB11p09340
[40]	HEUZE F E, 1983. High-temperature mechanical, physical and thermal properties of granitic rocks—a review[J]. International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, 20(1): 3-10.
[41]	HU H, ARGYROPOULOS S A, 1996. Mathematical modelling of solidification and melting: a review[J]. Modelling and Simulation in Materials Science and Engineering, 4(4): 371. doi: 10.1088/0965-0393/4/4/004
[42]	HUPPERT H E, SPARKS R S J, 1988. The generation of granitic magmas by intrusion of basalt into continental crust[J]. Journal of Petrology, 29(3): 599-624. doi: 10.1093/petrology/29.3.599
[43]	ITASCA CONSULTING GROUP INC, 2012. FLAC 3D Fast Lagrangian Analysis of Continua in 3 Dimensions—FLAC 3D help. Minneapolis, Minnesota.
[44]	KUMARI W G P, RANJITH P G, PERERA M S A, et al. , 2017. Mechanical behaviour of Australian Strathbogie granite under in-situ stress and temperature conditions: an application to geothermal energy extraction[J]. Geothermics, 65: 44-59. doi: 10.1016/j.geothermics.2016.07.002
[45]	LANGE R A, CASHMAN K V, NAVROTSKY A, 1994. Direct measurements of latent heat during crystallization and melting of a ugandite and an olivine basalt[J]. Contributions to Mineralogy and Petrology, 118(2): 169-181. doi: 10.1007/BF01052867
[46]	LESSEN M, 1956. Thermoelasticity and thermal shock[J]. Journal of the Mechanics and Physics of Solids, 5(1): 57-61. doi: 10.1016/0022-5096(56)90007-2
[47]	LI W T, HUANG B H, BI Z B, 2004. Thermal stress theory analysis and application[M]. Beijing: China Electric Power Press. (in Chinese)
[48]	LI Z H, CHI G X, BETHUNE K M, 2016. The effects of basement faults on thermal convection and implications for the formation of unconformity‐related uranium deposits in the Athabasca Basin, Canada[J]. Geofluids, 16(4): 729-751. doi: 10.2113/econgeo.112.2.451
[49]	LI Z H, CHI G X, BETHUNE K M, et al. , 2017. Structural controls on fluid flow during compressional reactivation of basement faults: insights from numerical modeling for the formation of unconformity-related uranium deposits in the Athabasca Basin, Canada[J]. Economic Geology, 112(2): 451-466.
[50]	LIENHARD V J H, LIENHARD IV J H, 2011. A heat transfer textbook[M]. 4th ed. Massachusetts: Phlogiston Press, 749.
[51]	LIU X C, XING H L, ZHANG D H, 2015. The mechanisms of the infill textures and its implications for the five-floor zonation at the Dajishan vein-type tungsten deposit, China[J]. Ore Geology Reviews, 65: 365-374. doi: 10.1016/j.oregeorev.2014.10.011
[52]	LIU X C, ZHANG D H, ZHAO B, et al. , 2017. Quantitative analysis of the “five-floor” vertical morphological zonation in the Piaotang tungsten deposits, South China[J]. Geological Journal of China Universities, 23(3): 408-416. (in Chinese with English abstract)
[53]	LIU X C, XIAO C H, ZHANG S H, et al. , 2020. Whether Sanguliu granite provided energy required for forming Wulong gold deposit, Liaoning Province, China?[J]. Earth Science, 45(11): 3998-4013. (in Chinese with English abstract)
[54]	LIU X C, ZHANG D H, YANG J W, et al. , 2023. High heat producing granites and prolonged extraction of tungsten and tin from melts[J]. Geochimica et Cosmochimica Acta, 348: 340-354. doi: 10.1016/j.gca.2023.03.012
[55]	LORD H W, SHULMAN Y, 1967. A generalized dynamical theory of thermoelasticity[J]. Journal of the Mechanics and Physics of Solids, 15(5): 299-309. doi: 10.1016/0022-5096(67)90024-5
[56]	MA C Q, LI Y Q, 2017. Incremental growth of granitoid plutons and highly crystalline magmatic differentiation[J]. Acta Petrologica Sinica, 33(5): 1479-1488. (in Chinese with English abstract)
[57]	MAO J W, XIE G Q, CHENG Y B, et al. , 2009. Mineral deposit models of Mesozoic ore deposits in South China[J]. Geological Review, 55(3): 347-354. (in Chinese with English abstract)
[58]	MATZEL J E P, BOWRING S A, MILLER R B, 2006. Time scales of pluton construction at differing crustal levels: examples from the Mount Stuart and Tenpeak intrusions, North Cascades, Washington[J]. Geological Society of America Bulletin, 118(11-12): 1412-1430. doi: 10.1130/B25923.1
[59]	MERRIMAN J D, WHITTINGTON A G, HOFMEISTER A M, et al. , 2013. Thermal transport properties of major Archean rock types to high temperature and implications for cratonic geotherms[J]. Precambrian Research, 233: 358-372. doi: 10.1016/j.precamres.2013.05.009
[60]	MIAO S Q, LI H P, CHEN G, 2014. Temperature dependence of thermal diffusivity, specific heat capacity, and thermal conductivity for several types of rocks[J]. Journal of Thermal Analysis and Calorimetry, 115(2): 1057-1063. doi: 10.1007/s10973-013-3427-2
[61]	MICHEL J, BAUMGARTNER L, PUTLITZ B, et al. , 2008. Incremental growth of the Patagonian Torres del Paine laccolith over 90 k. y. [J]. Geology, 36(6): 459-462. doi: 10.1130/G24546A.1
[62]	MÜLLER G, 1998. Experimental simulation of basalt columns[J]. Journal of Volcanology and Geothermal Research, 86(1-4): 93-96. doi: 10.1016/S0377-0273(98)00045-6
[63]	NABELEK P I, HOFMEOSTER A M, WHITTINGTON A G, 2012. The influence of temperature-dependent thermal diffusivity on the conductive cooling rates of plutons and temperature-time paths in contact aureoles[J]. Earth and Planetary Science Letters, 317-318: 157-164. doi: 10.1016/j.jpgl.2011.11.009
[64]	NAJAFI M, JALALI S M E, KHALOKAKAIE R, 2014. Thermal–mechanical–numerical analysis of stress distribution in the vicinity of underground coal gasification (UCG) panels[J]. International Journal of Coal Geology, 134-135: 1-16. doi: 10.1016/j.coal.2014.09.014
[65]	PETFORD N, CRUDEN A R, MCCAFFREY K J W, et al. , 2000. Granite magma formation, transport and emplacement in the Earth's crust[J]. Nature, 408(6813): 669-673. doi: 10.1038/35047000
[66]	POLYAKOVA I G, 2014. The main silica phases and some of their properties[M]//SCHMELZER J W P. Glass: selected properties and crystallization. Berlin: De Gruyter: 197-268.
[67]	QIN K Z, ZHAO J X, FAN H R, et al. , 2021. On the ore-forming depth and possible maximum vertical extension of the major type ore deposits[J]. Earth Science Frontiers, 28(3): 271-294. (in Chinese with English abstract)
[68]	RAGHAMI E, SCHRANK C, KRUHL J H, 2020. 3D modelling of the effect of thermal-elastic stress on grain-boundary opening in quartz grain aggregates[J]. Tectonophysics, 774: 228242. doi: 10.1016/j.tecto.2019.228242
[69]	SCAILLET B, PICHAVANT M, ROUX J, 1995. Experimental crystallization of leucogranite magmas[J]. Journal of Petrology, 36(3): 663-705. doi: 10.1093/petrology/36.3.663
[70]	SCAILLET B, HOLTZ F, PICHAVANT M, 2016. Experimental constraints on the formation of silicic magmas[J]. Elements, 12(2): 109-114. doi: 10.2113/gselements.12.2.109
[71]	SCHÖN J H, 2015. Physical properties of rocks: fundamentals and principles of petrophysics[M]. Amsterdam: Elsevier.
[72]	SCHÖPA A, ANNEN C, DILLES J H, et al. , 2017. Magma emplacement rates and porphyry copper deposits: thermal modeling of the Yerington Batholith, Nevada[J]. Economic Geology, 112(7): 1653-1672. doi: 10.5382/econgeo.2017.4525
[73]	SCHRANK C E, FUSSEIS F, KARRECH A, et al. , 2012. Thermal-elastic stresses and the criticality of the continental crust[J]. Geochemistry, Geophysics, Geosystems, 13(9): Q09005.
[74]	SONG Z X, QIAN X L, 1996. On the formation mechanism of granite: a review[J]. Geological Science and Technology Information, 15(3): 20-26. (in Chinese with English abstract)
[75]	STEIN C A, STEIN S, 1992. A model for the global variation in oceanic depth and heat flow with lithospheric age[J]. Nature, 359(6391): 123-129. doi: 10.1038/359123a0
[76]	TOSDAL R M, RICHARDS J P, 2001. Magmatic and structural controls on the development of porphyry Cu ± Mo ± Au deposits[M]//RICHARDS J P, TOSDAL R M. Structural controls on ore genesis. Society of Economic Geologists, 14: 157-181.
[77]	VOSTEEN H D, SCHELLSCHMIDT R, 2003. Influence of temperature on thermal conductivity, thermal capacity and thermal diffusivity for different types of rock[J]. Physics and Chemistry of the Earth, Parts A/B/C, 28(9-11): 499-509. doi: 10.1016/S1474-7065(03)00069-X
[78]	WANG D H, TANG J X, YING L J, et al. , 2010. Application of “Five levels + Basement” model for prospecting deposits into depth[J]. Journal of Jilin University (Earth Science Edition), 40(4): 733-738. (in Chinese with English abstract)
[79]	WANG D H, HUANG F, WANG Y, et al. , 2020a. Regional metallogeny of Tungsten-tin-polymetallic deposits in Nanling region, South China[J]. Ore Geology Reviews, 120: 103305. doi: 10.1016/j.oregeorev.2019.103305
[80]	WANG F, KONIETZKY H, 2019. Thermo-mechanical properties of granite at elevated temperatures and numerical simulation of thermal cracking[J]. Rock Mechanics and Rock Engineering, 52(10): 3737-3755. doi: 10.1007/s00603-019-01837-1
[81]	WANG F, KONIETZKY H, FRÜHWIRT T, et al. , 2020b. Laboratory testing and numerical simulation of properties and thermal-induced cracking of Eibenstock granite at elevated temperatures[J]. Acta Geotechnica, 15(8): 2259-2275. doi: 10.1007/s11440-020-00926-8
[82]	WANG X N, HUANG R Q, 1998. Influence of thermal stress on the surface stability of surrounding rock in a diversion tunnel[J]. Journal of Geological Hazards and Environment Preservation, 9(1): 43-48. (in Chinese with English abstract)
[83]	WEI X Y, LI Z H, DU P F, et al. , 2022. Application of numerical modeling in the study of fluid flow mechanism related to sandstone-type uranium deposits[J]. Uranium Geology, 38(1): 106-114. (in Chinese with English abstract)
[84]	WEIS P, DRIESNER T, HEINRICH C A, 2012. Porphyry-copper ore shells form at stable pressure-temperature fronts within dynamic fluid plumes[J]. Science, 338(6114): 1613-1616. doi: 10.1126/science.1225009
[85]	XING H L, MAKINOUCHI A, 2002. Three-dimensional finite element modeling of thermomechanical frictional contact between finite deformation bodies using R-minimum strategy[J]. Computer Methods in Applied Mechanics and Engineering, 191(37-38): 4193-4214. doi: 10.1016/S0045-7825(02)00372-9
[86]	XU J X, ZENG Z L, WANG D H, et al. , 2008. A new type of tungsten deposit in southern Jiangxi and the new model of "Five Floors + Basement" for prospecting[J]. Acta Geologica Sinica, 82(7): 880-887. (in Chinese with English abstract)
[87]	ŽÁK J, VYHNÁLEK B, KABELE P, 2006. Is there a relationship between magmatic fabrics and brittle fractures in plutons? A view based on structural analysis, anisotropy of magnetic susceptibility and thermo-mechanical modelling of the Tanvald pluton (Bohemian Massif) [J]. Physics of the Earth and Planetary Interiors, 157(3-4): 286-310. doi: 10.1016/j.pepi.2006.05.001
[88]	ZHANG D, LI F, HE J L, et al. , 2021. Mesozoic tectonic deformation and its rock / ore-control mechanism in the important metallogenic belts in South China [J]. Journal of Geomechanics, 27(4): 497-528. (in Chinese with English abstract)
[89]	ZHANG D H, JIN X D, MAO S D, et al. , 2011. The classification of ore-forming fluid and the efficiency of ore formation of magmatic hydrothermal solution[J]. Earth Science Frontiers, 18(5): 90-102. (in Chinese with English abstract)
[90]	ZHANG Q, JIN W J, LI C D, et al. , 2014. Magma-thermal field: its basic characteristics, and differences with geothermal field[J]. Acta Petrologica Sinica, 30(2): 341-349. (in Chinese with English abstract)
[91]	ZHANG S K, YU X F, JIA C, et al. , 2018. Effect study on thermal stress to weathering damage of dinosaur fossils[J]. Shandong Land and Resources, 34(5): 42-48. (in Chinese with English abstract)
[92]	ZHANG S S, 2011. Numerical simulation of magmatic hydrothermal system: a case study of Gejiu polymetallic mining district[D]. Wuhan: China University of Geosciences (Wuhan): 1-54. (in Chinese with English abstract)
[93]	ZHAO M C, YU X C, ZHANG Y F, et al. , 2020. Conceptual model for genesis of mineralized fissures in porphyry deposits and its geological significance[J]. Mineral Deposits, 39(1): 19-41. (in Chinese with English abstract)
[94]	ZHU Z N, YANG S Q, WANG R, et al. , 2022. Effects of high temperature on the linear thermal expansion coefficient of Nanan granite[J]. Acta Geodaetica et Geophysica, 57(2): 231-243. doi: 10.1007/s40328-022-00375-7
[95]	曹华文, 2015. 滇西腾-梁锡矿带中-新生代岩浆岩演化与成矿关系研究[D]. 北京: 中国地质大学（北京）: 1-340.
[96]	岑况, 田兆雪, 2012. 岩浆中心成矿系: 岩浆岩体和矿床组合的空间分带理想模式[J]. 现代地质, 26（5）: 1051-1057. doi: 10.3969/j.issn.1000-8527.2012.05.026
[97]	常成, 罗纲, 2022. 斑岩矿床侵入体顶部破裂系统形成的力学机制: 多场耦合数值模拟的启示[J]. 地球物理学报, 65（8）: 3006-3024. doi: 10.6038/cjg2022P0375
[98]	陈柏林, 高允, 2022. 江西德兴铜厂斑岩铜矿床细脉型矿体含矿裂隙系统研究[J]. 矿床地质, 41（6）: 1093-1107.
[99]	陈颙, 吴晓东, 张福勤, 1999. 岩石热开裂的实验研究[J]. 科学通报, 44（8）: 880-883. doi: 10.3321/j.issn:0023-074X.1999.08.022
[100]	陈育民, 徐鼎平, 2013. FLAC/FLAC 3D基础与工程实例[M]. 2版. 北京: 中国水利水电出版社.
[101]	范玉璐, 曹佳文, 余顺, 等, 2023. 高地应力作用下渭武高速木寨岭隧道围岩大变形灾变预测分析研究[J]. 地质力学学报, 29（6）: 786-800. doi: 10.12090/j.issn.1006-6616.2022110
[102]	方贵聪, 王登红, 冯佐海, 等, 2021. 华南石英脉型钨矿床扇状成矿的规律及其找矿意义[J]. 大地构造与成矿学, 45（3）: 523-533.
[103]	古德生, 李夕兵, 2003. 有色金属深井采矿研究现状与科学前沿[J]. 矿业研究与开发, 23（S1）: 1-5.
[104]	广东有色金属地质勘探公司九三二队, 1966. 我们是怎样用“五层楼”规律寻找、评价和勘探黑钨石英脉矿床的[J]. 地质与勘探（5）: 15-19.
[105]	韩学辉, 楚泽涵, 张元中, 2005. 岩石热开裂及其在工程学上的意义[J]. 石油实验地质, 27（1）: 98-100. doi: 10.3969/j.issn.1001-6112.2005.01.018
[106]	李维特, 黄保海, 毕仲波, 2004. 热应力理论分析及应用[M]. 北京: 中国电力出版社.
[107]	刘向冲, 张德会, 赵波, 等, 2017. 漂塘钨矿床“五层楼”垂直形态分带定量分析[J]. 高校地质学报, 23（3）: 408-416.
[108]	刘向冲, 肖昌浩, 张拴宏, 等, 2020. 辽东三股流岩体是否为五龙金矿成矿提供必要的能量?[J]. 地球科学, 45（11）: 3998-4013.
[109]	马昌前, 李艳青, 2017. 花岗岩体的累积生长与高结晶度岩浆的分异[J]. 岩石学报, 33（5）: 1479-1488.
[110]	毛景文, 谢桂青, 程彦博, 等, 2009. 华南地区中生代主要金属矿床模型[J]. 地质论评, 55（3）: 347-354. doi: 10.3321/j.issn:0371-5736.2009.03.005
[111]	秦克章, 赵俊兴, 范宏瑞, 等, 2021. 试论主要类型矿床的形成深度与最大延深垂幅[J]. 地学前缘, 28（3）: 271-294.
[112]	宋子新, 钱祥麟, 1996. 花岗岩成因机制研究综述[J]. 地质科技情报, 15（3）: 20-26.
[113]	王登红, 唐菊兴, 应立娟, 等, 2010. “五层楼+地下室”找矿模型的适用性及其对深部找矿的意义[J]. 吉林大学学报（地球科学版）, 40（4）: 733-738.
[114]	王贤能, 黄润秋, 1998. 引水隧洞工程中热应力对围岩表层稳定性的影响分析[J]. 地质灾害与环境保护, 9（1）: 43-48.
[115]	韦晓艳, 李增华, 杜鹏飞, 等, 2022. 数值模拟在砂岩型铀矿流体运移机制研究中的应用[J]. 铀矿地质, 38（1）: 106-114. doi: 10.3969/j.issn.1000-0658.2022.38.009
[116]	许建祥, 曾载淋, 王登红, 等, 2008. 赣南钨矿新类型及“五层楼+地下室”找矿模型[J]. 地质学报, 82（7）: 880-887. doi: 10.3321/j.issn:0001-5717.2008.07.003
[117]	张达, 李芳, 贺晓龙, 等, 2021. 华南重要成矿区带中生代构造变形及其控岩控矿机理[J]. 地质力学学报, 27（04）: 497-528.
[118]	张德会, 金旭东, 毛世德, 等, 2011. 成矿热液分类兼论岩浆热液的成矿效率[J]. 地学前缘, 18（5）: 90-102.
[119]	张旗, 金惟俊, 李承东, 等, 2014. 岩浆热场: 它的基本特征及其与地热场的区别[J]. 岩石学报, 30（2）: 341-349.
[120]	张尚坤, 于学峰, 贾超, 等, 2018. 热应力对恐龙化石风化损坏的影响研究[J]. 山东国土资源, 34（5）: 42-48. doi: 10.3969/j.issn.1672-6979.2018.05.005
[121]	张嵩松, 2011. 岩浆热液成矿系统的数值模拟: 以云南个旧锡多金属矿区为例[D]. 武汉: 中国地质大学（武汉）: 1-54.
[122]	赵茂春, 余先川, 张翼飞, 等, 2020. 斑岩型矿床容矿裂隙成因的几种概念模型及其意义[J]. 矿床地质, 39（1）: 19-41.

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