Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Teh-Ching Liu"'
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 32, Iss 3, Pp 319-338 (2021)
The Baima igneous complex (BIC) consists of a cumulate layered gabbroic unit, an Fe-Ti oxide ore zone, and an isotropic quartz syenite. The formation of the BIC is attributed to a variety of petrological processes including: silicate immiscibility, f
Externí odkaz:
https://doaj.org/article/7927c1344f5f4f2694678e315de9c1f8
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 21, Iss 2, p 267 (2010)
A gab bro from Chintan, Sindian, was subjected to experiments at atmospheric pressure to study the fractional crystallization of the gabbroic melt. The range of experimental temperatures was from 1120 to 1262°C, and the durations were from about 16
Externí odkaz:
https://doaj.org/article/fa0418e5662d4025aa4eb6fdd92d4cad
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 17, Iss 1, p 233 (2006)
Granite from the transition zone of the Huang Yang Dam in the Qilian orogenic belt, NW China, is studied using a high-temperature furnace at atmospheric condition. Twenty-two runs are made to locate the liquidus temperature, the solidus temperature,
Externí odkaz:
https://doaj.org/article/521084f65a6c41a8b66ac3c0cab641b7
Autor:
Yu-Ho Li, Huei-Fen Chen, Hsiao-Tien Hung, Jhih-Hao Jiang, Ying-Lai Tsai, Eugene Huang, Jianng-Neng Fang, Teh-Ching Liu
Publikováno v:
Minerals, Vol 11, Iss 167, p 167 (2021)
Minerals
Volume 11
Issue 2
Minerals
Volume 11
Issue 2
In this work, Raman spectroscopic experiments are conducted on zeolites, including a total of 33 varieties and seven groups with different secondary structural frameworks, for which characteristic vibration modes are studied. Most of the zeolites sho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::92041a610a424fc8e3d5a97c1a173215
https://doi.org/10.3390/min11020167
https://doi.org/10.3390/min11020167
Publikováno v:
Quaternary International. 349:221-231
To investigate whether quartz can be crystallized from the magma at the Chilungshan andesite in Northern Taiwan, melting experiments involving 17 runs were performed at atmospheric pressure. The liquidus temperature was determined to be 1285 °C, and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::712fe73a0da84f7e44654e4e8abffc6a
https://doi.org/10.1016/j.quaint.2014.06.037
https://doi.org/10.1016/j.quaint.2014.06.037
Publikováno v:
Mineralogy & Petrology. Mar2009, Vol. 95 Issue 3/4, p327-340. 14p. 1 Diagram, 3 Charts, 7 Graphs.
Publikováno v:
Mineralogy and Petrology. 95:327-340
This study measures the reaction rate of dolomite and aragonite (calcite) into Mg-calcite at 800, 850, and 900°C and 1.6 GPa. The dry synthetic dolomite-aragonite aggregate transformed very rapidly into dolomite-calcite polycrystalline aggregate whi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c85d085cf6bd9e225c2639e7bcae34aa
https://doi.org/10.1007/s00710-008-0036-z
https://doi.org/10.1007/s00710-008-0036-z
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 21, Iss 2, p 267 (2010)
A gab bro from Chintan, Sindian, was subjected to experiments at atmospheric pressure to study the fractional crystallization of the gabbroic melt. The range of experimental temperatures was from 1120 to 1262°C, and the durations were from about 16
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eeabdfc6dd3fd57439e286e712f69d02
https://doaj.org/article/fa0418e5662d4025aa4eb6fdd92d4cad
https://doaj.org/article/fa0418e5662d4025aa4eb6fdd92d4cad
Publikováno v:
Geophysical Research Letters. 18:1397-1400
Ultrasonic measurements of compressional wave velocities for six komatiitic melts containing 13–30 wt% MgO are reported in the frequency range 3–20 MHz and in the temperature range 1280–1661°C. Melts with less than about 20 wt% MgO have veloci
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ff658d97bd6415cbc9a2f5caa087d32
https://doi.org/10.1029/91gl01803
https://doi.org/10.1029/91gl01803
Autor:
Teh-Ching Liu, Dean C. Presnall
Publikováno v:
Contributions to Mineralogy and Petrology. 104:735-742
Liquidus phase relationships determined on the join anorthite-forsterite-quartz at 20 kbar show primary phase fields for quartz (q), forsterite (fo), enstatite (en), spinel (sp), anorthite (an), sapphirine (sa), and corundum (cor). Increasing pressur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c8797b4587235963b0e95004e6e020b3
https://doi.org/10.1007/bf01167290
https://doi.org/10.1007/bf01167290