biển tiến

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The Vietnamese term "biển tiến" refers to a geological process known as "marine transgression" in English. This occurs when sea levels rise and water covers previously exposed land areas. It is a significant concept in geography and geology, often related to changes in the Earth's climate and sea levels over time.

Usage Instructions:

• "Biển tiến" is used primarily in discussions about geography, geology, and environmental science. It is not a term you would typically use in everyday conversation unless discussing related topics.

Example:

• "Trong lịch sử địa chất, biển tiến đã tạo ra nhiều lớp trầm tích trên bề mặt trái đất." (In geological history, marine transgression has created many sediment layers on the Earth's surface.)

Advanced Usage:

• When studying sedimentology or paleoenvironments, "biển tiến" can be analyzed in relation to other processes such as "biển thoái" (marine regression), which refers to the opposite process where sea levels fall and land is exposed.

Word Variants:

• "Biển tiến" can be used in different contexts by combining it with other words. For instance:
  • "Biển tiến và biển thoái" (Marine transgression and regression)
  • "Thời kỳ biển tiến" (Period of marine transgression)

Different Meanings:

• While "biển tiến" specifically refers to marine transgression in a geological context, it does not have other common meanings. It is a specialized term.

Academic

1. (địa lý) Marine transgression