마그마가 화성을 붉게 만든다

화성의 내부 구조에 대한 예술가의 번역을 보여주는 애니메이션. 크레딧: NASA/JPL-Caltech

Mars Interior Exploration using Seismic Investigations, Geodesy and Heat Transport (InSight) launched in May 2018 and safely landed on the Martian surface in November of that same year. Its two-year mission was to study the deep interior of Mars to learn how celestial bodies with rocky surfaces, such as the Earth and the Moon, formed. It recently recorded a record-setting, monster quake on Mars, but sadly, it is almost lights out for InSight.

One of InSight’s key tools for that mission is Seismic Experiment for Interior Structure (SEIS). This round, dome-shaped instrument takes the “pulse” or seismic vibrations of Mars. Using data from SEIS, scientists have made a new discovery about marsquakes.

Volcanic activity beneath the surface of Mars could be responsible for triggering repetitive marsquakes, which are similar to earthquakes, in a specific region of the Red Planet, scientists from The Australian National University (ANU) suggest.

New research published in Nature Communications shows scientists from ANU and the Chinese Academy of Sciences in Beijing have discovered 47 previously undetected marsquakes beneath the Martian crust in an area called Cerberus Fossae — a seismically active region on Mars that is less than 20 million years old.

“It can help us answer fundamental questions about the solar system and the state of Mars’ core, mantle and the evolution of its currently lacking magnetic field.”

The authors of the study speculate that magma activity in the Martian mantle, which is the inner layer of Mars sandwiched between the crust and the core, is the cause of these newly detected marsquakes.

The findings suggest magma in the Martian mantle is still active and is responsible for the volcanic marsquakes, contrary to past beliefs held by scientists that these events are caused by Martian tectonic forces.

According to geophysicist and co-author Professor Hrvoje Tkalcic, from the ANU Research School of Earth Sciences, the repetitive nature of these quakes and the fact they were all detected in the same area of the planet suggests Mars is more seismically active than scientists previously thought.

“We found that these marsquakes repeatedly occurred at all times of the Martian day, whereas marsquakes detected and reported by NASA in the past appeared to have occurred only during the dead of night when the planet is quieter,” Professor Tkalcic said.

“Therefore, we can assume that the movement of molten rock in the Martian mantle is the trigger for these 47 newly detected marsquakes beneath the Cerberus Fossae region.”

Professor Tkalcic said the continuous seismicity suggests the Cerberus Fossae region on Mars is “seismically highly active.”

“Knowing that the Martian mantle is still active is crucial to our understanding of how Mars evolved as a planet,” he said.

“It can help us answer fundamental questions about the solar system and the state of Mars’ core, mantle and the evolution of its currently-lacking magnetic field.”

The researchers used data collected from a seismometer attached to NASA’s InSight lander, which has been collecting data about marsquakes, Martian weather, and the planet’s interior since landing on Mars in 2018.

Using a unique algorithm, the researchers were able to apply their techniques to the NASA data to detect the 47 previously undiscovered marsquakes.

The study authors say while the quakes would have caused some shaking on Mars, the seismic events were relatively small in magnitude and would barely be felt if they had occurred on Earth. The quakes were detected over a period of about 350 sols — a term used to refer to one solar day on Mars — which is equivalent to about 359 days on Earth.

According to Professor Tkalcic, the marsquake findings could help scientists figure out why the Red Planet no longer has a magnetic field.

“The marsquakes indirectly help us understand whether convection is occurring inside of the planet’s interior, and if this convection is happening, which it looks like it is based off our findings, then there must be another mechanism at play that is preventing a magnetic field from developing on Mars,” he said.

“All life on Earth is possible because of the Earth’s magnetic field and its ability to shield us from cosmic radiation, so without a magnetic field life as we know it simply wouldn’t be possible.

“Therefore, understanding Mars’ magnetic field, how it evolved, and at which stage of the planet’s history it stopped is obviously important for future missions and is critical if scientists one day hope to establish human life on Mars.”

Reference: “Repetitive marsquakes in Martian upper mantle” by Weijia Sun and Hrvoje Tkalcic, 30 March 2022, Nature Communications.
DOI: 10.1038/s41467-022-29329-x

READ  켄터키주 렉싱턴시는 우주 비행사에게 우주 여행 공고를 제출하도록 초대합니다.
답글 남기기

이메일 주소는 공개되지 않습니다. 필수 필드는 *로 표시됩니다

You May Also Like

32명의 새로운 사망자와 3,891명의 새로운 양성 사례 – 마감일

일요일: 일요일, 그리고 천사 카운티 공중 보건국은 10명의 새로운 사망자를 보고했습니다. 코로나…

전 국가 안보위원회 관계자는 COVID-19 발병에 대한 WHO의 조사가“대부분 모니터링 ”되었다고 말했습니다.

대서양위원회의 한 고위 연구원이 자산에 대한 주요 국제 조사를 요청했습니다. 코로나 바이러스…

웨스트 나일 바이러스는 올해 매사추세츠의 모기 샘플에서 처음 발견되었습니다.

매사추세츠 공중 보건부는 웨스트 나일 바이러스가 올해 처음으로 매사추세츠의 모기에서 발견되었다고 밝혔다.…

금성에 연결된 NASA 장비는 혹독한 날씨에 대처할 준비를 합니다.

NASA 과학자들은 적절하게 명명된 DAVINCI(또는 Venus Deep Exploration of Noble Gases, Chemistry…