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8.1級!美國世紀大地震橫在加州門口

(2010-10-10 14:33:23) 下一個
斷層帶通過的農莊,地表一片祥和,但斷層在空照下,卻也顯露醜陋麵貌,隨時會摧毀家園。(取自美國地質調查所等網站) 地震專家8日發布爆炸性學術報告:對南加州威脅最大的聖安德裏斯斷層(San Andreas fault),地震周期為88年,比傳統學說縮短兩倍。

專家說,芮氏規模8.1地震已近在南加州人家門口!

貫穿南北加州的聖安德裏斯斷層,多年來被地震專家視為「加州安全的定時炸彈」,何時大地震,地震學家多年來較一致的說法,是250至450年一次,規模7.8左右。

但由爾灣加大和亞利桑納州立大學共同研究多年、8日發表在權威學術雜誌「Geology」的最新報告指出,聖安德裏斯斷層下次地震規模很可能高達8.1,破壞力可能北從蒙特瑞縣(Monterey County)通達南加州沙頓海(Salton Sea),總長340哩。 「多年來地震學家一直同意聖安德裏斯斷層的活動周期為200年至250年之間,精確說法為234年」,南加大地震學家酈永剛表示,此一結論是採用航天觀測地震後地表壕溝及錯位深度,通過網格推算而產生。最新研究是採用雷射探測和光學掃描,發現更精確的震後痕跡,很小的錯位也能發現,因此發現在聖安德裏斯最近一次地震前,曾發生多次8.0左右的大地震。

據加州地震檔桉記載,聖安德裏斯斷層對南加威脅最大的最近一次地震發生在1857年,規模7.9,震央在北加州蒙特瑞縣附近泰洪堡(Fort Tejon),向南延伸200哩,在洛杉磯縣北部天使國家森林一帶,轉而向東延伸到聖伯納汀諾縣的Cajon Pass,靠近現在的15號公路附近。 據記載,那次地震前後搖動三分鍾左右,導致土壤液化,部分地區下沉嚴重,一些地區樹木連根拔起。不過由於當時洛杉磯地居民隻有4000人左右,損失有限。

之後迄今150年,聖安德裏斯斷層南段,即橫跨洛杉磯西北100哩卡瑞索(Carrizo)平原,一直保持休眠狀態。 不過通過新的雷射和光學技術最新研究顯示,在1857年前,聖安德裏斯斷層在1417、1462、1565、1614、1713年都曾發生過規模8左右的大地震,隻是那時沒有人住院醫治,沒有留下紀錄。 參與本次研究的爾灣加大地震學家Lisa GrantLudwig表示,過去大家一直喊「狼來了」,在她看來,「現在狼真的要來啦」。

南加州地震中心主任Thomas Jordan也相信,「被捆綁且超負荷的聖安德裏斯巨人,現在隨時都會爆發」。不過酈永剛教授認為,聖安德裏斯斷層近期會發生8.0以上地震的說法尚有爭議。他認為,近年南加州發生8.0以上地震可能性為50%,發生7.0以上地震機率為99.5%。

酈永剛表示,由於不久前海地和墨西哥相繼出現7.8以上地震,使威脅南加南部的墨西哥灣斷層釋放出一定能量,來自南部的地震威脅可能推遲幾年;而如果按88年周期的理論,南加州也早已超過周期。 「值得注意的是,震度每差一級,震幅相差十倍,但釋放的能量卻相差32倍」,酈永剛指出,墨西哥灣地震大概隻釋放積壓能量的六分之一左右,民眾對大地震的防備,仍不可掉以輕心。

(世界日報 2010-10-10)

San Andreas fault capable of magnitude 8.1 earthquake over 340-mile swath of California, researchers say [Updated]

October 8, 2010 

San andreas The "Big One" on the San Andreas fault just got a little bigger.

New research showing a section of the fault is long overdue for a major earthquake has some scientists saying that the fault is capable of a magnitude 8.1 earthquake that could run 340 miles from Monterey County to the Salton Sea. 

Whether such a quake would happen in our lifetime had been a subject of hot debate among scientists. That's because experts had believed that a major section of the southern San Andreas, which runs through the Carrizo Plain 100 miles northwest of Los Angeles, would remain dormant for at least another century.

But that rosy hypothesis seemed to be shattered by a recent report in the journal Geology, which said that even that section of the San Andreas is far overdue for the "Big One." [Updated, Oct. 9: The report, published in August, was written by Sinan Akciz and Lisa Grant Ludwig of UC Irvine, and J. Ramon Arrowsmith and Olaf Zielke of Arizona State University.]

Now, according to U.S. Geological Survey seismologist Lucy Jones, it is entirely possible that all 340 miles of the southern San Andreas could be ready to erupt at any time. Such a scenario would trigger a magnitude 8.1 earthquake, said Thomas Jordan, director of the Southern California Earthquake Center, a calculation with which Jones agreed.

"All of it has plenty enough stress for it to be ready to go," Jones said. "The biggest implication of [the report] is that it increases the likelihood that when we do have a big earthquake, it will grow into the 'wall-to-wall' rupture."

[Updated, Oct. 9: Such a temblor could cause much more damage because with a longer stretch of the fault rupturing, a larger area is exposed to the quake, and the shaking would last longer.]

The walls Jones is referring to are the boundaries of the southern San Andreas, which begins in the Salton Sea and ends in the town of Parkfield in Monterey County. Scientists consider the southern San Andreas fault as one segment generally because it behaves the same -- it rarely rumbles, but when awakened, the shaking can be devastating.

In contrast, the section of the San Andreas north of Parkfield up to Hollister in San Benito County behaves differently. That section constantly moves at a creep -- meaning stress is relieved regularly, so large quakes don't occur there.

Large quakes haven't occurred anywhere on the southern San Andreas for more than a century, making it a sleeping giant that has been building stress for so long it could snap at any moment.

"My concern is that we will get a series of large earthquakes along the San Andreas fault," Jordan said. The last "Big One" to rip through Southern California occurred in 1857, when an estimated magnitude-7.9-quake, ruptured 200 miles of fault between Monterey and San Bernardino counties. It wasn't a wall-to-wall quake: It stopped near the Cajon Pass, near the present-day 15 Freeway, probably because the fault south of it shook just a few decades earlier, in 1812, Jones said. Because the 1812 quake had relieved tectonic tension in that area, it effectively put a brake to the 1857 quake from moving further south.

But with the San Bernardino County section of the fault now having accumulated two centuries' worth of strain, there may not be any brakes now. "Can I imagine the 1857 earthquake happening again and stopping at the Cajon Pass? Probably not," Jones said. "Once you have a big slip, you're more likely to move along down the fault," Jones said. "If the rupture has been made ... that’s a lot of momentum that will keep the rupture moving down the fault."

The San Andreas has long been considered one of the most dangerous faults in Southern California because of its length. Not only do longer faults produce bigger quakes, they emit a type of shaking energy that can travel longer distances.

"So a much larger area is affected by a really large earthquake," Jones said.

In 2008, seismologists developed a scenario for a large earthquake on the San Andreas -- a magnitude 7.8 shaker that begins at the Salton Sea and barrels northwest along the fault toward San Bernardino and Los Angeles counties.

-- Rong-Gong Lin II

Photo: Quake researchers study a portion of the San Andreas fault. Ricardo DeAratanha / Los Angeles Times; Map: U.S. Geological Survey



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