کتابخانه دیجیتال دانشگاه هنر اصفهان | Deglaciated areas of Kilimanjaro as a source of volcanic trace elements deposited on the ice cap during the late Holocene.

Deglaciated areas of Kilimanjaro as a source of volcanic trace elements deposited on the ice cap during the late Holocene.

پدیدآورنده

نام

Deglaciated areas of Kilimanjaro as a source of volcanic trace elements deposited on the ice cap during the late Holocene.

زبان اثر

انگلیسی

شناسگر

10.1007/s11146-009-9166-2 (شماره مدرک)

10.1016_j.quascirev.2014.03.007 (importid)

ناشر

تاریخ انتشار

2014

قالب (کتاب)

کتاب