“多旋回地形”的概念、定义、翻译、参考文献-科学参考

单词	多旋回地形
释义	多旋回地形 Encyclopedia 理学多旋回地形释 polycyclic landform多旋回地形在地形发育过程中，由于地壳运动或自然环境的变化，使内、外营力及其作用强度发生多次变化所形成的地形。又称多循环地形、多轮回地形。
随便看	University of al-Quaraouiyine university of applied sciences university of applied technology University of Auckland University of Basel University of Bergen University of Bologna University of British Colombia University of British Columbia University of British Columbia and Laval University Telescope University of British Columbia Museum of Anthropology University of Buenos Aires University of Calcutta University of California University of California libraries University of Cambridge University of Cape Town University of Chicago University of Coimbra University of Copenhagen University of Dakar University of Dar es Salaam University of Delhi University of East Africa University of Edinburgh

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