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北大西洋に隣接する大陸の修正されたトライアス紀末期の緯度
1Department of Geological Sciences, Rutgers University, Piscataway, NJ 08854, USA. dvk@rci.rutgers.edu
まとめ
この研究は,地磁気モデルを使用して古代の岩石の傾きエラーを修正します. 結果は,トリアシク後期に安定した二極場が存在していたことを確認し,パンゲアがより速く漂っていたことを明らかにし,広大な赤道湿気帯が存在していたことを示唆している.
科学分野:
- 古代磁気学と地力学について
- 初期のメソゾーイク時代の地球科学
背景:
- 傾き誤差は,堆積岩の古磁気研究における一般的な問題である.
- 地球の古代の磁場を理解することは,古代地理学の再構築に不可欠です.
研究 の 目的:
- 初期メソゾイク期の堆積岩の傾き誤差を修正するための統計的方法を開発し,適用する.
- トライアス後期におけるパンゲアの古磁場と古緯度の再構築.
主な方法:
- 統計的地磁場モデルを使用して,傾斜の誤差を特定し,修正しました.
- 検証のために,修正された堆積岩データと独立した岩石データとを比較した.
- 構造板の移動と気候帯を推論するために,古緯度データを分析した.
主要な成果:
- 北米,グリーンランド,欧州の堆積岩の傾き誤差を正した.
- トライアス紀後期における地球中心の軸対極場の動作を実証した.
- パンゲアのこの地域では,100万年あたり ~0.6度というより速い極方向漂流率を計算しました.
結論:
- 地中枢軸二極体フィールドモデルは,トライアス紀後期に信頼性があります.
- パンゲアは,メソゾイク初期に重要な緯度漂移を経験した.
- トライアス紀後期の赤道湿帯は,現在の帯の幅に匹敵していた.
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