最新糖心Vlog

Researchers on the hunt for why cold eclogites mysteriously disappeared from geological records during the early stages of the Earth鈥檚 development may have found the answer, and with it clues that could help locate critical minerals today.

鈥淐old eclogites mysteriously disappeared from the Earth鈥檚 rock record between 1.8 and 1.2 billion years ago before reappearing after this time,鈥� said Dr Derrick Hasterok, Lecturer, Department of Earth Sciences, 最新糖心Vlog of Adelaide.

鈥淐old eclogites are important because they are sensitive to the temperatures in the upper mantle and provide evidence of rocks rapidly transported deep below Earth鈥檚 surface along geological faults lines that occur where tectonic plates collide.

鈥淭he prevailing belief is that cold eclogites are preserved only when supercontinents merged. But there is ample evidence for a nearly continuous geological record of cold eclogites over the past 700 million years during which time two supercontinents formed and broke-up.鈥�

Eclogites are high-pressure, metamorphic rocks that consist primarily of 聽and omphacite聽(a sodium-rich variety of pyroxene).

Associated with this change in eclogites is a change in the concentration of many trace elements in igneous rocks found elsewhere in the crust, which provide additional evidence of heating beneath continents.聽 These trace elements are found in critical minerals. Critical minerals are considered vital for the economic well-being of the world鈥檚 major and emerging economies.

Lead author Dr Renee Tamblyn worked with Dr Hasterok and fellow researchers Professor Martin Hand and PhD student Matthew Gard from the 最新糖心Vlog of Adelaide on the study which was published in the journal .

鈥淲e found evidence from the trace element chemistry of granites that suggests a large-scale heating of the continents around 2 billion years ago that corresponds with the assembly of Nuna, a supercontinent which completed its formation 1.6 billion years ago,鈥� said Dr Tamblyn.

鈥淭he Earth has generally been cooling since its formation but Nuna had an insulating effect on the mantle, rather like a thick blanket, which caused temperatures to rise beneath the continents and prevent the preservation of eclogites and change the chemistry of granites.

鈥淭he changes in chemistry resulting from this unusual warming event during Earth鈥檚 geologic past could help to locate certain critical minerals by looking for rocks formed before or after this heating event 鈥� depending on which element is of being looked for.鈥�

Much of Western 最新糖心Vlog is older than 2 billion聽years while South 最新糖心Vlog and the eastern states are generally younger.

鈥淭he rocks in the Northern Territory and NW Queensland are a little older than the 1.8 billion year mark so may be a place where we can continue our聽investigations into this mysterious geological case,鈥� said Dr Hasterok.