The formation of P-rich Fe–Ti oxide ore layers in the Taihe layered intrusion, SW China: Implications for magma-plumbing system process

2014 ◽  
Vol 57 ◽  
pp. 539-559 ◽  
Author(s):  
Yu-Wei She ◽  
Song-Yue Yu ◽  
Xie-Yan Song ◽  
Lie-Meng Chen ◽  
Wen-Qin Zheng ◽  
...  
2018 ◽  
Vol 6 ◽  
Author(s):  
Takeshi Kuritani ◽  
Azusa Yamaguchi ◽  
Sayuki Fukumitsu ◽  
Mitsuhiro Nakagawa ◽  
Akiko Matsumoto ◽  
...  

2018 ◽  
Vol 123 (10) ◽  
pp. 8615-8636
Author(s):  
Masashi Ushioda ◽  
Eiichi Takahashi ◽  
Morihisa Hamada ◽  
Toshihiro Suzuki ◽  
Kenji Niihori

2021 ◽  
Author(s):  
Yabin Li ◽  
Aihua Weng ◽  
et al.

Details on the 3-D magnetotelluric inversion, sensitivity test of resistivity anomalies and melt fraction estimation, and Figures S1–S11. <br>


Lithos ◽  
2020 ◽  
Vol 354-355 ◽  
pp. 105274 ◽  
Author(s):  
Amir Eskandari ◽  
Reza Deevsalar ◽  
Rosanna De Rosa ◽  
Ryuichi Shinjo ◽  
Paola Donato ◽  
...  

2020 ◽  
Vol 11 (1) ◽  
Author(s):  
M. R. Patrick ◽  
B. F. Houghton ◽  
K. R. Anderson ◽  
M. P. Poland ◽  
E. Montgomery-Brown ◽  
...  

Abstract The 2018 summit and flank eruption of Kīlauea Volcano was one of the largest volcanic events in Hawaiʻi in 200 years. Data suggest that a backup in the magma plumbing system at the long-lived Puʻu ʻŌʻō eruption site caused widespread pressurization in the volcano, driving magma into the lower flank. The eruption evolved, and its impact expanded, as a sequence of cascading events, allowing relatively minor changes at Puʻu ʻŌʻō to cause major destruction and historic changes across the volcano. Eruption forecasting is inherently challenging in cascading scenarios where magmatic systems may prime gradually and trigger on small events.


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