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(单词翻译:双击或拖选)
By David McAlary
Washington
15 February 2007
A U.S. spacecraft has provided fresh evidence that water once flowed on Mars. In this case, it is water that ran deep underground through rock fissures1, places where scientists say life could have thrived hidden from the harsh Martian surface environment. VOA's David McAlary reports.
Satellite photo showing erosion of rock formations on Mars
The U.S. space agency NASA's newest satellite around the red planet, the Mars Reconnaissance Orbiter, has taken color pictures showing a landscape called Chasma Canyon2 composed of dozens of alternating layers of dark and light toned rocks and crossed by dark sand dunes3.
Within those layers, the detailed4 images show fractures, called joints5, surrounded by light colored bedrock that was once deep underground before erosion exposed it. University of Arizona researcher Chris Okubo argues that this brighter bedrock is clear evidence that a liquid flowed through it and washed the dark minerals away, as water has done in similar situations on Earth.
"So the unaltered rock has this dark brown color. However, along the joints you see that the dark brown minerals have been chemically removed by the fluids that were flowing within the joints, so the area has been bleached," he said.
Chris Okubo
In a paper in the journal Science, Okubo and a colleague say the bleaching6 would have taken a long time to occur - perhaps hundreds of millions or a few billion years. He explained at a scientific meeting in San Francisco that an underground setting for water could have been conducive7 for life on Mars.
"The fact that these areas were underground is important because the overlying several kilometers of rock would have acted as buffers8 against any sort of harsh environmental conditions that may have existed at the surface of Mars at this time. So these areas would be nice protected areas for any sort of biologic processes to occur," he said.
Previous findings by NASA robot rovers on Mars have shown that water once flowed on the surface and may have formed lakes and even oceans. Recent photos of fresh gullies from another U.S. satellite indicate it might still be percolating9 up from underground.
Mars water specialist Stephen Clifford of the Lunar and Planetary Institute in Houston, Texas, says Okubo's research supports the notion that ground water remains10 beneath the Martian surface crust.
"The fact that there is such persuasive11 evidence of joints and fractures in the crust also suggests that this groundwater had an ability to flow enormous distances. That has implications for understanding the processes that led to the redistribution of water from surface environments like lakes and seas into the subsurface, into that increasingly thick layer of frozen ground that was the result of both the external climate cooling and the decline of the planet's internal heat flow," he said.
Okubo says his analysis awaits confirmation12 by a future generation of Mars rovers, which could check the chemical composition of the rocks up close.
1 fissures | |
n.狭长裂缝或裂隙( fissure的名词复数 );裂伤;分歧;分裂v.裂开( fissure的第三人称单数 ) | |
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2 canyon | |
n.峡谷,溪谷 | |
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3 dunes | |
沙丘( dune的名词复数 ) | |
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4 detailed | |
adj.详细的,详尽的,极注意细节的,完全的 | |
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5 joints | |
接头( joint的名词复数 ); 关节; 公共场所(尤指价格低廉的饮食和娱乐场所) (非正式); 一块烤肉 (英式英语) | |
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6 bleaching | |
漂白法,漂白 | |
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7 conducive | |
adj.有益的,有助的 | |
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8 buffers | |
起缓冲作用的人(或物)( buffer的名词复数 ); 缓冲器; 减震器; 愚蠢老头 | |
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9 percolating | |
n.渗透v.滤( percolate的现在分词 );渗透;(思想等)渗透;渗入 | |
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10 remains | |
n.剩余物,残留物;遗体,遗迹 | |
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11 persuasive | |
adj.有说服力的,能说得使人相信的 | |
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12 confirmation | |
n.证实,确认,批准 | |
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