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| 来源： | Freesound 前往原页面 查看译文 |
| 作者： | RTB45 |
| 许可： | CC0 公众共享许可协议 |
| 描述： | Mud Volcano Field, DavisSchrimpf Seep Field, Salton Sea, California Lat: 33.20070326716746Lon: 244.42179501054162 The DavisSchrimpf onshore seep field site in the Salton Sea geothermal system is the result of shallow magmatic intrusions in a sedimentary basin. The SSGS is situated in the Salton Trough in southern California, an area with abundant surface manifestations of hydrothermal activity. The hydrothermal system in the Salton Trough occurs in a pullapart setting where rifting and associated magmatic intrusions are responsible for the strong heat flow. One of the most concentrated and wellexpressed onshore seep fields is the DavisSchrimpf field, where more than 50 individual seeps are located in this area. Gas venting from gryphons and pools is vigorous with a continuous bubbling activity. Water and mud mixtures are continuously expelled down the flanks of the gryphons. Carbon dioxide produced from devolatilization reactions involving sedimentary carbonate is the main driver for the seep activity. The morphological features of the Davis Schrimpf seep field are strikingly similar to seep fields on dormant mud volcanoes However, the DavisSchrimpf seeps are not related to mud volcanism, as mud volcanism normally implies largescale mud breccia eruptions and a low temperature seep stage. From the; JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114, B09201, doi:10.1029/2008JB006247, 2009 |
| 标签： | DavisSchrimpf volcano mudpot hotsprings carbondioxide SaltonSea bubbles boiling water fluid eruption hydrothermal gas fieldrecording boil bubble simmer California field lava mud geyser gurgle hotspring bubbling seep volcanic vent |
| 音频格式 | wav |
| 声音时长 | 04:08 |
| 文件大小 | 41.8 MB |
| 比特率 | 1409 kbps |
| 采样率 | 44100 Hz |
| 位深度 | 16 bit |
| 声道 | 立体声 |