Magma Reservoir Below Laguna del Maule Volcanic Field, Chile, Imaged With Surface-Wave Tomography
文献类型：期刊论文
| 作者 | Wespestad, Crystal E.1; Thurber, Clifford H.1; Andersen, Nathan L.2; Singer, Brad S.1; Cardona, Carlos3; Zeng, Xiangfang4; Bennington, Ninfa L.1; Keranen, Katie5; Peterson, Dana E.5; Cordell, Darcy6 |
| 刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
 |
| 出版日期 | 2019-03-01 |
| 卷号 | 124期号:3页码:2858-2872 |
| 关键词 | Laguna del Maule surface-wave tomography magma reservoir ambient noise |
| ISSN号 | 2169-9313 |
| DOI | 10.1029/2018JB016485 |
| 英文摘要 | The Laguna del Maule (LdM) volcanic field comprises the greatest concentration of postglacial rhyolite in the Andes and includes the products of 40km(3) of explosive and effusive eruptions. Recent observations at LdM by interferometric synthetic aperture radar and global navigation satellite system geodesy have revealed inflation at rates exceeding 20cm/year since 2007, capturing an ongoing period of growth of a potentially large upper crustal magma reservoir. Moreover, magnetotelluric and gravity studies indicate the presence of fluids and/or partial melt in the upper crust near the center of inflation. Petrologic observations imply repeated, rapid extraction of rhyolitic melt from crystal mush stored at depths of 4-6km during at least the past 26ka. We utilize multiple types of surface-wave observations to constrain the location and geometry of low-velocity domains beneath LdM. We present a three-dimensional shear-wave velocity model that delineates a 450-km(3) shallow magma reservoir 2 to 8km below surface with an average melt fraction of 5%. Interpretation of the seismic tomography in light of existing gravity, magnetotelluric, and geodetic observations supports this model and reveals variations in melt content and a deeper magma system feeding the shallow reservoir in greater detail than any of the geophysical methods alone. Geophysical imaging of the LdM magma system today is consistent with the petrologic inferences of the reservoir structure and growth during the past 20-60kyr. Taken together with the ongoing unrest, a future rhyolite eruption of at least the scale of those common during the Holocene is a reasonable possibility. |
| 资助项目 | National Science Foundation Integrated Earth Systems program[EAR-141179] |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000464922800037 |
| 出版者 | AMER GEOPHYSICAL UNION |
| 源URL | [http://202.127.146.157/handle/2RYDP1HH/7120]  |
| 专题 | 中国科学院武汉植物园 |
| 通讯作者 | Thurber, Clifford H. |
| 作者单位 | 1.Univ Wisconsin, Dept Geosci, Madison, WI 53706 USA 2.Univ Oregon, Dept Earth Sci, Eugene, OR 97403 USA 3.Observ Volcanol Andes Sur, Serv Nacl Geol & Mineria, Temuco, Chile 4.Chinese Acad Sci, Inst Geodesy & Geophys, State Key Lab Geodesy & Earths Dynam, Wuhan, Hubei, Peoples R China 5.Cornell Univ, Dept Earth & Atmospher Sci, Ithaca, NY USA 6.Univ Alberta, Dept Phys, Edmonton, AB, Canada 7.GNS Sci, Taupo, New Zealand 8.Simon Fraser Univ, Dept Earth Sci, Ctr Nat Hazards Res, Burnaby, BC, Canada |
| 推荐引用方式 GB/T 7714 | Wespestad, Crystal E.,Thurber, Clifford H.,Andersen, Nathan L.,et al. Magma Reservoir Below Laguna del Maule Volcanic Field, Chile, Imaged With Surface-Wave Tomography[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2019,124(3):2858-2872. |
| APA | Wespestad, Crystal E..,Thurber, Clifford H..,Andersen, Nathan L..,Singer, Brad S..,Cardona, Carlos.,...&Williams-Jones, Glyn.(2019).Magma Reservoir Below Laguna del Maule Volcanic Field, Chile, Imaged With Surface-Wave Tomography.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,124(3),2858-2872. |
| MLA | Wespestad, Crystal E.,et al."Magma Reservoir Below Laguna del Maule Volcanic Field, Chile, Imaged With Surface-Wave Tomography".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 124.3(2019):2858-2872. |
入库方式： OAI收割
来源：武汉植物园
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