這本雙月刊涵蓋了變質(zhì)研究的全部范圍，從單個(gè)晶體的尺度到巖石圈板塊的尺度。《變質(zhì)地質(zhì)學(xué)雜志》匯集了變質(zhì)巖石學(xué)、礦床地質(zhì)學(xué)、地球化學(xué)、構(gòu)造學(xué)和構(gòu)造地質(zhì)學(xué)等領(lǐng)域的科學(xué)家，至今仍與17年前創(chuàng)刊時(shí)一樣具有創(chuàng)新性。自創(chuàng)辦以來(lái)，該雜志一直與幾個(gè)協(xié)會(huì)有聯(lián)系，包括:地質(zhì)學(xué)會(huì)(英國(guó));歐洲地球科學(xué)聯(lián)盟;美國(guó)礦物學(xué)學(xué)會(huì);加拿大礦物學(xué)協(xié)會(huì);澳大利亞地質(zhì)學(xué)會(huì)。

This bimonthly title encompasses the entire range of metamorphic studies, from the scale of individual crystals to that of lithospheric plates. Bringing together scientists working in metamorphic petrology, mineral deposit geology, geochemistry, tectonics, and structural geology, the Journal of Metamorphic Geology remains as innovative today as it was seventeen years ago when it began. Since its inception, the Journal has been associated with several societies including: The Geological Society (UK); The European Union of Geosciences; The Mineralogical Society of America; The Canadian Mineralogical Association; The Geological Society of Australia.