During the X Italian Antarctic expedition (1994/95), 639 rocks have been sampled within the aim of the international EUROSHACK project in Shackleton Range. They include intrusive, subvolcanic, volcanic and metamorphic rocks. The investigated regions are within Shackleton Range SU 26-30/1* USGS sheet. Project: International Antarctic Geological Expedition to the Shackleton Range 1994/95.

During the XXXIII and XXXIV Italian Antarctic expeditions (2017/18, 2018/19), 194 rocks have been sampled within the aim of the project "Dating of tectonic activity along the Transantarctic Mountains front" in northern and southern Victoria Land. They include intrusive, subvolcanic, volcanic, metamorphic and sedimentary rocks. The investigated regions are within Convoy Range ST 57-60/1, Franklin Island ST 57-60/2*, Mount Joyce SS 55-57/16, Mount Melbourne SS 58-60/9, Reeves Névé SS 55-57/12, Relief Inlet SS 58-60/13 and Ross Island ST 57-60/6* USGS sheets.

During the X Italian Antarctic expedition (1994/95), 42 rocks have been sampled within the aim of the project "Geological survey and sampling of Jurassic volcanics" in northern Victoria Land. They include subvolcanic and volcanic rocks. The investigated regions are within Mount Joyce SS 55-57/16 USGS sheet.

During the XV Italian Antarctic expedition (1999/2000), 213 rocks have been sampled within the aim of the BACKTAM project in Oates Land and George V Land. They include intrusive, subvolcanic, volcanic, metamorphic and sedimentary rocks. The investigated regions are within Australian Antarctic Territory - Ross Dependency - Sr57-58, Australian Antarctic Territory - Sq55-56, Australian Antarctic Territory - Sr55-56 and Australian Antarctic Territory - Terre Adelie - Sq53-54 sheets. Project: Backside of the Transantarctic Mountains.

During the XVIII Italian Antarctic expedition (2002/03), 63 rocks have been sampled within the aim of the project "Geological mapping of Victoria Land" in northern and southern Victoria Land. They include intrusive, subvolcanic, volcanic, metamorphic and sedimentary rocks and sands. The investigated regions are within Convoy Range ST 57-60/1, Freyberg Mountains SS 58-60/1, Mount Joyce SS 55-57/16, Mount Melbourne SS 58-60/9, Reeves Névé SS 55-57/12 and Sequence Hills SS 55-57/8 USGS sheets.

This dataset includes all the carbonaceous chondrites CV group collected during the Italian Antarctic Expeditions since 1997 in Victoria Land and now preserved at the repository of the Museo Nazionale dell’Antartide.

This dataset includes all the iron meteorites (achondrites) collected during the Italian Antarctic Expeditions since 1991 in Victoria Land and now preserved at the repository of the Museo Nazionale dell’Antartide.

This dataset includes all the lodranite meteorites (primitive achondrites) collected during the Italian Antarctic Expeditions since 1991 in Victoria Land and now preserved at the repository of the Museo Nazionale dell’Antartide.

During the XIX Italian Antarctic expedition (2003/04), 100 rocks have been sampled within the aim of the WIBEM project in northern Victoria Land. They include intrusive, subvolcanic and metamorphic rocks. The investigated regions are within Daniels Range SR 57-58/14, Sequence Hills SS 55-57/8 and Welcome Mountain SS 55-57/4 USGS sheets. Project: WIBEM (Wilkes Basin Eastern Margin): geophysical exploration of the eastern margin of the Wilkes Basin.

During the XV and XVI Italian Antarctic expeditions (1999/2000, 2000/01), 609 rocks have been sampled within the aim of the project "Tectono-metamorphic and magmatic evolution of the Antarctic Pacific paleo-margin of Gondwana in the late Proterozoic-Early Paleozoic (Victoria Land, Shackleton Range, Dronning Maud Land)" in northern Victoria Land and central Transantarctic Mountains. They include intrusive, subvolcanic and metamorphic rocks. The investigated regions are within Mount Melbourne SS 58-60/9, Mount Murchison SS 58-60/5, Reeves Névé SS 55-57/12, Sequence Hills SS 55-57/8, Welcome Mountain SS 55-57/4, Cape Selborne SU 55-60/2 and Mount Olympus SU 56-60/1 USGS sheets.