中文簡(jiǎn)介

地球流體為研究流體在地殼礦物化學(xué)和結(jié)構(gòu)演化中的作用提供了一個(gè)國(guó)際論壇。它的明確目標(biāo)是在進(jìn)行地球流體研究的各個(gè)子學(xué)科之間傳播思想。為此目的，將鼓勵(lì)作者強(qiáng)調(diào)其研究的跨學(xué)科相關(guān)性，并使來(lái)自其他子學(xué)科的讀者盡可能接近他們的工作。地球流體強(qiáng)調(diào)整個(gè)地殼地下流體的化學(xué)和物理方面(盡管不包括硅酸鹽熔體)。地球流體包括地下水、陸地或海底地?zé)崃黧w、盆地鹵水、石油變質(zhì)水或巖漿流體的研究，但需要與在地質(zhì)時(shí)間尺度上具有重要意義的過(guò)程相關(guān)聯(lián)。鼓勵(lì)作者提交描述理論或觀測(cè)研究的文章，探索地下流體的地質(zhì)地球化學(xué)或地球物理屬性，量化對(duì)滲透性地球化學(xué)輸運(yùn)和熱輸運(yùn)的地質(zhì)控制，或記錄地殼流體行為的應(yīng)用方面。

　　英文簡(jiǎn)介

Geofluids provides an international forum for original research into the role of fluids in mineralogical chemical and structural evolution of the Earth's crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end authors will be encouraged to stress the transdisciplinary relevance of their research and to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes both chemical and physical aspects of subsurface fluids throughout the Earth's crust (although excluding silicate melts). Geofluids spans studies of groundwater terrestrial or submarine geothermal fluids basinal brines petroleum metamorphic waters or magmatic fluids but requires relevance to processes that are significant on a geological time scale. Authors are encouraged to submit articles that describe theoretical or observational studies explore the geologic geochemical or geophysical attributes of subsurface fluids quantify the geologic controls on permeability geochemical transport and heat transport or document applied aspects of crustal fluid behaviour.

　　近年期刊自引率趨勢(shì)圖

　　JCR分區(qū)

JCR分區(qū)等級(jí)	JCR所屬學(xué)科	分區(qū)	影響因子
Q2	GEOLOGY	Q2	2.006
	GEOCHEMISTRY & GEOPHYSICS	Q3

　　近年期刊影響因子趨勢(shì)圖

　　CiteScore數(shù)值

CiteScore	SJR	SNIP	學(xué)科類別	分區(qū)	排名	百分位
2.20	0.372	0.713	大類：Earth and Planetary Sciences 小類：General Earth and Planetary Sciences	Q2	94 / 191	51%

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