Geothermal gradient and heat flow of the Erlian Basin and adjacent areas, Northern China: Geodynamic implication
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Shaopeng Huang | Yi Li | Yong-shui Zhou | Yinhui Zuo | Tingting Ke | Jiong Zhang | W. Xu | R. Yu
[1] Shaopeng Huang,et al. Terrestrial heat flow in the baiyinchagan sag, erlian Basin, northern China , 2020 .
[2] W. Xu,et al. Terrestrial heat flow and lithospheric thermal structure in the Chagan Depression of the Yingen‐Ejinaqi Basin, north central China , 2020, Basin Research.
[3] H. Shaopeng,et al. Measurement and analysis of the thermal conductivities of rock samples from the Baiyinchagan Sag and Uliastai Sag, Erlian Basin, northern China , 2020 .
[4] Jian Wang,et al. Crustal structure beneath Northeast China from ambient noise tomography , 2019, Physics of the Earth and Planetary Interiors.
[5] W. Xiao,et al. Thermo-tectonic history of the Junggar Alatau within the Central Asian Orogenic Belt (SE Kazakhstan, NW China): Insights from integrated apatite U/Pb, fission track and (U–Th)/He thermochronology , 2019, Geoscience Frontiers.
[6] Tianmeng Yuan. Geoelectric structure of the collision zone between the Siberia plate and the North China Craton and Discussion on the deep Suture Boundary , 2019, Acta Geologica Sinica - English Edition.
[7] L. Shuai,et al. Post-Triassic multiple exhumation of the Taihang Mountains revealed via low-T thermochronology: Implications for the paleo-geomorphologic reconstruction of the North China Craton , 2019, Gondwana Research.
[8] J. Lei,et al. Pn anisotropic tomography of Northeast China and its implications to mantle dynamics , 2019, Journal of Asian Earth Sciences.
[9] Yizuo Shi,et al. Terrestrial heat flow of continental China: Updated dataset and tectonic implications , 2019, Tectonophysics.
[10] Wei Xu,et al. Present-day geothermal regime of the Uliastai Depression, Erlian Basin, North China , 2018, Energy Exploration & Exploitation.
[11] I. Sevostianov,et al. Replacement relations for thermal conductivity of a porous rock , 2017 .
[12] B. Jahn,et al. The Mongol-Okhotsk Ocean subduction-related Permian peraluminous granites in northeastern Mongolia: Constraints from zircon U-Pb ages, whole-rock elemental and Sr-Nd-Hf isotopic compositions , 2017 .
[13] Lijuan He. Wet plume atop of the flattening slab: Insight into intraplate volcanism in East Asia , 2017 .
[14] Jie Tang,et al. Early Mesozoic southward subduction history of the Mongol–Okhotsk oceanic plate: Evidence from geochronology and geochemistry of Early Mesozoic intrusive rocks in the Erguna Massif, NE China , 2016 .
[15] S. Wilde,et al. The late Paleozoic to Mesozoic evolution of the eastern margin of the Central Asian Orogenic Belt in China , 2015 .
[16] S. Wilde. Final amalgamation of the Central Asian Orogenic Belt in NE China: Paleo-Asian Ocean closure versus Paleo-Pacific plate subduction — A review of the evidence , 2015 .
[17] A. Kozlovsky,et al. Late Mesozoic–Cenozoic intraplate magmatism in Central Asia and its relation with mantle diapirism: Evidence from the South Khangai volcanic region, Mongolia , 2015 .
[18] Zhilong Huang,et al. Characteristics and origin of lacustrine source rocks in the Lower Cretaceous, Erlian Basin, northern China , 2015 .
[19] S. Wilde,et al. Continental flood basalts derived from the hydrous mantle transition zone , 2015, Nature Communications.
[20] C. Yuan,et al. A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia: Oroclines, Sutures, and Terminal Accretion , 2015 .
[21] C. Jaupart,et al. Heat Flow and Thermal Structure of the Lithosphere , 2015 .
[22] Qi Jiaf. The distribution of Early Cretaceous faulted-sags and their relationship with basement structure within Erlian Basin , 2015 .
[23] Lijuan He. Thermal regime of the North China Craton: Implications for craton destruction , 2015 .
[24] N. Qiu,et al. Geothermal evidence of Meso-Cenozoic lithosphere thinning in the Jiyang sub-basin, Bohai Bay Basin, eastern North China Craton , 2014 .
[25] Kerry T.B. MacQuarrie,et al. Climate change impacts on groundwater and soil temperatures in cold and temperate regions: Implications, mathematical theory, and emerging simulation tools , 2014 .
[26] W. Xiao,et al. Early Paleozoic to Middle Triassic bivergent accretion in the Central Asian Orogenic Belt: insights from zircon U-Pb dating of ductile shear zones in central Inner Mongolia, China , 2014 .
[27] Xiao-dong Liu,et al. Sedimentology, stratigraphy and palynological occurrences of the late Cretaceous Erlian Formation, Erlian Basin, Inner Mongolia, People's Republic of China , 2014 .
[28] Huaichun Wu,et al. Crustal structures revealed from a deep seismic reflection profile across the Solonker suture zone of the Central Asian Orogenic Belt, northern China: An integrated interpretation , 2014 .
[29] M. Santosh,et al. Seismic imaging of the deep structure under the Chinese volcanoes: An overview , 2013 .
[30] Wenliang Xu,et al. Spatial–temporal relationships of Mesozoic volcanic rocks in NE China: Constraints on tectonic overprinting and transformations between multiple tectonic regimes , 2013 .
[31] Kevin P. Furlong,et al. Heat Flow, Heat Generation, and the Thermal State of the Lithosphere , 2013 .
[32] S. Wilde,et al. The crustal accretion history and tectonic evolution of the NE China segment of the Central Asian Orogenic Belt , 2013 .
[33] P. Jian,et al. Carboniferous and Cretaceous mafic–ultramafic massifs in Inner Mongolia (China): A SHRIMP zircon and geochemical study of the previously presumed integral “Hegenshan ophiolite” , 2012 .
[34] Zhao Yong. Mantle sources and magma genesis of Quaternary volcanic rocks in the Halaha River and Chaoer River area,Great Xing'an Range , 2012 .
[35] R. Lowell,et al. Modeling heat transfer from a convecting, crystallizing, replenished silicic magma chamber at an oceanic spreading center , 2011 .
[36] E. Burov. Rheology and strength of the lithosphere , 2011 .
[37] S. Wilde,et al. Geochronology of the Phanerozoic granitoids in northeastern China , 2011 .
[38] S. Wilde,et al. Early Paleozoic metamorphic rocks of the Erguna block in the Great Xing'an Range, NE China: Evidence for the timing of magmatic and metamorphic events and their tectonic implications , 2011 .
[39] Fan Qi. Studies on Quaternary volcanism stages of Halaha river and Chaoer river area in the Great Xing'an Range:Evidence from K-Ar dating and volcanic geology features , 2011 .
[40] Ilmutdin M. Abdulagatov,et al. Effect of pressure, temperature, and oil-saturation on the thermal conductivity of sandstone up to 250 MPa and 520 K , 2010 .
[41] Z. Tao. Spatial and Temporal Distribution of Granitoids in the Middle Segment of the Sino-Mongolian Border and Its Tectonic and Metallogenic Implications , 2010 .
[42] A. Hasegawa,et al. The dynamics of big mantle wedge, magma factory, and metamorphic–metasomatic factory in subduction zones , 2009 .
[43] I. M. Abdulagatov,et al. Effect of temperature and pressure on the thermal conductivity of sandstone , 2009 .
[44] Dapeng Zhao,et al. Multiscale seismic tomography and mantle dynamics , 2009 .
[45] Bin Chen,et al. Evolution of the Solonker suture zone: Constraints from zircon U–Pb ages, Hf isotopic ratios and whole-rock Nd–Sr isotope compositions of subduction- and collision-related magmas and forearc sediments , 2009 .
[46] Pan Gui-tang. Subdivision of tectonic units in China , 2009 .
[47] Georg Dresen,et al. Rheology of the Lower Crust and Upper Mantle: Evidence from Rock Mechanics, Geodesy, and Field Observations , 2008 .
[48] S. Wilde,et al. Geochemistry of Permian bimodal volcanic rocks from Central Inner Mongolia, North China: Implication for Tectonic setting and Phanerozoic continental growth in Central Asian Orogenic Belt , 2008 .
[49] B. Zhi. Quaternary Volcano Cluster of Wulanhada,Right-back-banner,Chahaer,Inner Mongolia. , 2008 .
[50] Dunyi Liu,et al. Zircon SHRIMP U-Pb ages of the “Xinghuadukou Group” in Hanjiayuanzi and Xinlin areas and the “Zhalantun Group” in Inner Mongolia, Da Hinggan Mountains , 2007 .
[51] Brian F. Windley,et al. Tectonic models for accretion of the Central Asian Orogenic Belt , 2007, Journal of the Geological Society.
[52] L. Rybach,et al. Heat flow, heat transfer and lithosphere rheology in geothermal areas: Features and examples , 2005 .
[53] Tian,et al. Yanshan, Gaoshan——Two Active Volcanoes of the Volcanic Cluster in Arshan, Inner Mongolia , 2005 .
[54] Yi Shi-wei. Characteristic of Geotherm-Geopressure System in Erlian Basin , 2004 .
[55] Dunyi Liu,et al. Zircon SHRIMP geochronology of the Xinkailing-Kele complex in the northwestern Lesser Xing’an Range, and its geological implications , 2004 .
[56] C. Koeberl,et al. Geochemistry of metasomatised spinel peridotite xenoliths from the Dariganga Plateau, South-eastern Mongolia , 2002 .
[57] Lijuan He,et al. COMPILATION OF HEAT FLOW DATA IN THE CHINA CONTINENTAL AREA (3rd edition) , 2001 .
[58] Walter D. Mooney,et al. Thermal thickness and evolution of Precambrian lithosphere: A global study , 2001 .
[59] Bin Chen,et al. Two contrasting paleozoic magmatic belts in northern Inner Mongolia, China: petrogenesis and tectonic implications , 2000 .
[60] Shaopeng Huang,et al. Temperature trends over the past five centuries reconstructed from borehole temperatures , 2000, Nature.
[61] W. McDonough,et al. Thermal structure, thickness and composition of continental lithosphere , 1998 .
[62] J. Shao,et al. Geological effects in tectonic superposition of Paleo-Pacific domain and Paleo-Asian domain in northern part of North China , 1997 .
[63] Giorgio Ranalli,et al. Rheology of the lithosphere in space and time , 1997, Geological Society, London, Special Publications.
[64] R. Haenel. Geothermal Investigations in the Rhenish Massif , 1983 .