emanate
发表于 2025-3-21 20:06:28
书目名称Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin影响因子(影响力)<br> http://figure.impactfactor.cn/if/?ISSN=BK0383334<br><br> <br><br>书目名称Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin影响因子(影响力)学科排名<br> http://figure.impactfactor.cn/ifr/?ISSN=BK0383334<br><br> <br><br>书目名称Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin网络公开度<br> http://figure.impactfactor.cn/at/?ISSN=BK0383334<br><br> <br><br>书目名称Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin网络公开度学科排名<br> http://figure.impactfactor.cn/atr/?ISSN=BK0383334<br><br> <br><br>书目名称Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin被引频次<br> http://figure.impactfactor.cn/tc/?ISSN=BK0383334<br><br> <br><br>书目名称Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin被引频次学科排名<br> http://figure.impactfactor.cn/tcr/?ISSN=BK0383334<br><br> <br><br>书目名称Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin年度引用<br> http://figure.impactfactor.cn/ii/?ISSN=BK0383334<br><br> <br><br>书目名称Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin年度引用学科排名<br> http://figure.impactfactor.cn/iir/?ISSN=BK0383334<br><br> <br><br>书目名称Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin读者反馈<br> http://figure.impactfactor.cn/5y/?ISSN=BK0383334<br><br> <br><br>书目名称Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin读者反馈学科排名<br> http://figure.impactfactor.cn/5yr/?ISSN=BK0383334<br><br> <br><br>
DEFT
发表于 2025-3-22 00:19:39
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Fallibility
发表于 2025-3-22 01:29:35
Saralinsky Graben—Devonian Rift of the Kuznetsk-Minusinsk Zone, Altai–Sayan Folded Areaa Geological Surveys in the 1950s–80s. The research was aimed at characterizing the grabens, and other structures of the region, and any associated ore mineralization and geochemical anomalies. Summaries of this early research are reported in Mustafin et al. (.), Kryukov et al. (.) and Turchenko (.)
凝乳
发表于 2025-3-22 06:01:56
Guide for Field Geology of the Lower Devonian Byskar Series on the Educational Geological Ground of y, covers a vast area (~5,000 km.) on the eastern slope of the Kuznetsk Alatau, partly of the Bateniov Ridge and the North Minusinsk depression of the Minusinsk Intermountain Trough (Parnachev and Vasilyev .). In the mountainous areas there are many geological features of a huge age range—from Prote
贵族
发表于 2025-3-22 10:34:12
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allergen
发表于 2025-3-22 13:46:41
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allergen
发表于 2025-3-22 19:26:16
https://doi.org/10.1007/978-3-663-01296-2A large number of subvolcanic bodies cut through Devonian and Carboniferous volcanogenic and sedimentary rocks within the territory of North-Minusinsk depression (Fig. 1). These subvolcanic bodies belong to two magmatic associations.
DRAFT
发表于 2025-3-23 00:05:38
Die soziale Ordnung des GrundgesetzesThe geological section of Bolshoi Ilek, southeast of Western Siberia, represented by Cretaceous and Quaternary systems has been reassessed. Its major part is composed of the Lower Cretaceous deposits of deltic genesis that reached 80-m thickness and characterized the Ilek Formation stratotype.
Psychogenic
发表于 2025-3-23 01:57:23
https://doi.org/10.1007/978-3-531-92002-3In the central part of the Altai-Sayan folded region (ASFR), intensive post-collisional continental magmatism of increased alkalinity has long been known. The products of this magmatism are widely distributed, both in the basal part of the Minusinsk basin section and in the smaller superimposed structures within their fold structures.
浪费时间
发表于 2025-3-23 06:32:44
Die soziale Praxis des GerichtsverfahrensNumerous recently obtained geochronological data on the metamorphic and magmatic associations of the western part of the CAFB permitted distinguishing the Early Ordovician accretion-collision stage (490–450 Ma) in the development of this megastructure (Fig. 1).