Whole-rock 40Ar/39Ar geochronology, geochemistry, and stratigraphy of intraplate Cenozoic volcanic rocks, central Mongolia

被引:28
作者
Ancuta, Leonard D. [1 ]
Zeitler, Peter K. [1 ]
Idleman, Bruce D. [1 ]
Jordan, Brennan T. [2 ]
机构
[1] Lehigh Univ, Dept Earth & Environm Sci, Bethlehem, PA 18015 USA
[2] Univ South Dakota, Dept Sustainabil & Environm, Vermillion, SD 57069 USA
基金
美国国家科学基金会;
关键词
LARGE IGNEOUS PROVINCES; MANTLE STRUCTURE; HANGAY DOME; BENEATH; SIBERIA; INVERSION; HOTSPOTS; ORIGIN; REGION; DELAMINATION;
D O I
10.1130/B31788.1
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A new comprehensive suite of 235 whole-rock 40Ar/39Ar ages ranges from Holocene to ca. 30 Ma for Cenozoic volcanic rocks in central Mongolia. Their total preserved volume is similar to 1540 km(3), but prior to erosion, the volume may have been as high as 2900 km(3). The 235 new stratigraphically referenced ages, combined with surface mapping, suggest that volcanic output began to increase in the early Miocene and peaked in the middle Miocene, with a gradual decrease in volume through the Holocene. Trace-element inversion modeling suggests that the volcanic rocks were derived by low degrees of partial melting of a garnet lherzolite source at a depth greater than 62 km. The low total volumes and the lack of an apparent age-progressive hotspot track suggest that the volcanism cannot be attributed to a deep mantle plume beneath central Mongolia. The long-term gradual increase and subsequent decrease in volcanic output may also rule out delamination as the cause of the volcanism. Instead, we favor a small-scale mantle upwelling to explain the cause of the intraplate volcanism in the region. This upwelling could have been the result of one or more different processes, including edge-driven convection, redirection of asthenospheric flow by the thick lithosphere of the Siberian craton to the north, shear-driven upwelling, delamination, drips, or upwelling related to stagnant slabs in the mantle transition zone.
引用
收藏
页码:1397 / 1408
页数:12
相关论文
共 65 条
[1]   Large igneous provinces, delamination, and fertile mantle [J].
Anderson, DL .
ELEMENTS, 2005, 1 (05) :271-275
[2]   Non-hotspot volcano chains produced by migration of shear-driven upwelling toward the East Pacific Rise [J].
Ballmer, Maxim D. ;
Conrad, Clinton P. ;
Smith, Eugene I. ;
Harmon, Nicholas .
GEOLOGY, 2013, 41 (04) :479-482
[3]   Upper mantle flow beneath and around the Hangay dome, Central Mongolia [J].
Barruol, Guilhem ;
Deschamps, Anne ;
Deverchere, Jacques ;
Mordvinova, Valentina V. ;
Ulziibat, Munkhuu ;
Perrot, Julie ;
Artemiev, Alexandre A. ;
Dugarmaa, Tundev ;
Bokelmann, Goetz H. R. .
EARTH AND PLANETARY SCIENCE LETTERS, 2008, 274 (1-2) :221-233
[4]   Helium isotopes provide no evidence for deep mantle involvement in widespread Cenozoic volcanism across Central Asia [J].
Barry, T. L. ;
Ivanov, A. V. ;
Rasskazov, S. V. ;
Demonterova, E. I. ;
Dunai, T. J. ;
Davies, G. R. ;
Harrison, D. .
LITHOS, 2007, 95 (3-4) :415-424
[5]   Petrogenesis of Cenozoic basalts from Mongolia: Evidence for the role of asthenospheric versus metasomatized lithospheric mantle sources [J].
Barry, TL ;
Saunders, AD ;
Kempton, PD ;
Windley, BF ;
Pringle, MS ;
Dorjnamjaa, D ;
Saandar, S .
JOURNAL OF PETROLOGY, 2003, 44 (01) :55-91
[6]  
Barry TL, 1998, GEODYNAMICS, V27, P347
[7]  
Caves JK, 2014, AM J SCI, V314, P1171, DOI [10.2475/08.2014.011, 10.2475/08.2014.01]
[8]   Mantle-driven uplift of Hangai Dome: New seismic constraints from adjoint tomography [J].
Chen, Min ;
Niu, Fenglin ;
Liu, Qinya ;
Tromp, Jeroen .
GEOPHYSICAL RESEARCH LETTERS, 2015, 42 (17) :6967-6974
[9]   Holocene Volcanism in Central Mongolia and Northeast China: Asynchronous Decompressional and Fluid Melting of the Mantle [J].
Chuvashova, I. S. ;
Rasskazov, S. V. ;
Yasnygina, T. A. ;
Saranina, E. V. ;
Fefelov, N. N. .
JOURNAL OF VOLCANOLOGY AND SEISMOLOGY, 2007, 1 (06) :372-396
[10]   LARGE IGNEOUS PROVINCES - CRUSTAL STRUCTURE, DIMENSIONS, AND EXTERNAL CONSEQUENCES [J].
COFFIN, MF ;
ELDHOLM, O .
REVIEWS OF GEOPHYSICS, 1994, 32 (01) :1-36