/* DATA DESCRIPTION:
Citation:	Guo, Kun; Wang, Xiaoyuan; Chen, Shuai (2021): In situ elemental, Sr isotope composition of plagioclase and elemental composition of clinopyroxene and thermobarometric data of andesite from Kueishantao, north of Taiwan, China [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.929297
Abstract:	This dataset reports in situ major and trace elements, Sr isotopic ratios of plagioclase and in situ major and trace elements of clinopyroxene of andesite from Kueishantao, north of Taiwan, China. The andesite belongs to the subalkaline, tholeiitic and calc-alkaline magma series. The phenocryst minerals in andesites from KST account for 80-90% of the whole-rock samples, including plagioclase, cinlopyroxene, orthopyroxene, Fe-Ti oxides, zircon and apatite. Major element compositions of Pl and Cpx were obtained with a JEOL JXA-8230 electron microprobe at Ocean University of China. Trace element compositions were obtained with LA-ICP-MS at the Wuhan Sample Solution Analytical Technology Co., Ltd. Sr isotope ratios of Pl were measured by a Neptune Plus MC-ICP-MS (Thermo Fisher Scientific, Bremen, Germany) in combination with a GeoLas HD excimer ArF laser ablation system (Coherent, Göttingen, Germany) at the Wuhan Sample Solution Analytical Technology Co., Ltd. Considering all geochemical, 87Sr/86Sr isotope and geophysical constraints, the principal magma source of KST andesites was probably the lower continental crust, which foundered into the convecting mantle and subsequently melted and interacted with asthenospheric mantle materials. A full discussion of the results can be found in the related article.
Keyword(s):	andesite; clinopyroxene; in-situ mineral geochemistry; in-situ Sr isotope; plagioclase
Related to:	Guo, Kun; Wang, Xiaoyuan; Chen, Shuai; Shang, Luning; Liu, Bingquan; Zhang, Xia (2022): The delamination of lower crust in continental back-arc basin: Evidence from Sr isotope and elemental compositions of plagioclase and clinopyroxene in andesites from Kueishantao, north of Taiwan, China. Lithos, 106653, https://doi.org/10.1016/j.lithos.2022.106653
Coverage:	MEDIAN LATITUDE: 24.834484 * MEDIAN LONGITUDE: 121.961951 * SOUTH-BOUND LATITUDE: 24.834120 * WEST-BOUND LONGITUDE: 121.961940 * NORTH-BOUND LATITUDE: 24.834900 * EAST-BOUND LONGITUDE: 121.961960
	DATE/TIME START: 2011-05-11T00:00:00 * DATE/TIME END: 2011-05-11T00:00:00
License:	Creative Commons Attribution 4.0 International (CC-BY-4.0) (URI: https://creativecommons.org/licenses/by/4.0/)
Size:	7 datasets
*/
/* TABULAR SUMMARY OF DATASETS LISTED IN THIS COLLECTION: */
Filename	Citation of child dataset
S1_Pl_comp.tab	Guo, Kun; Wang, Xiaoyuan; Chen, Shuai (2021): Major element compositions of the plagioclases from andesites from the Kueishantao island analysed by EMPA (S1). https://doi.org/10.1594/PANGAEA.929272
S2_Pl_comp_zoned.tab	Guo, Kun; Wang, Xiaoyuan; Chen, Shuai (2021): Major element zoned compositions of the plagioclases from andesites from the Kueishantao island analysed by EMPA (S2). https://doi.org/10.1594/PANGAEA.929273
S3_Pl_trace_elem.tab	Guo, Kun; Wang, Xiaoyuan; Chen, Shuai (2021): Trace element compositions of the plagioclases from andesites from the Kueishantao island analysed by LA-ICP-MS (S3). https://doi.org/10.1594/PANGAEA.929276
S4_Pl_Sr_isotopes.tab	Guo, Kun; Wang, Xiaoyuan; Chen, Shuai (2021): In-situ Sr isotopes for plagioclase from andesites from the Kueishantao island analysed by LA-MC-ICP-MS (S4). https://doi.org/10.1594/PANGAEA.929279
S5_Cpx_comp.tab	Guo, Kun; Wang, Xiaoyuan; Chen, Shuai (2021): Major element compositions of the clinopyroxenes from andesites from the Kueishantao island analysed by EMPA (S5). https://doi.org/10.1594/PANGAEA.929284
S6_Cpx_trace_elem.tab	Guo, Kun; Wang, Xiaoyuan; Chen, Shuai (2021): Trace element compositions of the clinopyroxene from andesites from the Kueishantao island analysed by LA-ICP-MS (S6). https://doi.org/10.1594/PANGAEA.929289
S7_Whole_rock.tab	Guo, Kun; Wang, Xiaoyuan; Chen, Shuai (2021): Major element compositions of the whole rocks from the Kueishantao island (S7). https://doi.org/10.1594/PANGAEA.929294
