And the first excavation was conducted in the 60s by The Deccan College, Puna.

普纳的德干学院 (The Deccan College) 在 60 年代进行了第一次挖掘。

Another location, the Deccan region of India, one of the most volcanic areas during the late Cretaceous, provides more evidence.

印度的德干地区是另一个相关地点，这里是白垩纪晚期火山活动最为频繁的地区之一，这个地区提供了更多证据。

In the Deccan plateau in western India, there are more than two million cubic kilometers of lava, some of it 2,400 meters thick, formed over 500,000 years of slurping eruption.

在印度西部的 D 高原，存在着超过 2 百万立方千米的岩浆，有的地方厚度达到 2 400米，这些都是在超过 50 万年的缓慢喷发后形成的。

We know that there was a long series of volcanic eruptions at the end-Cretaceous because there are huge lava fields of the right age in India called the Deccan Traps.

我们知道在白垩纪末期发生了一连串的火山喷发，因为印度有巨大的适龄熔岩区，称为德干地陷。

Other theories propose that volcanic activity, particularly in the Deccan Traps in present-day India, spewed vast amounts of sulfur and carbon dioxide into the atmosphere, leading to acid rain and a greenhouse effect.

其他理论认为，火山活动，特别是当今印度德干地盾的火山活动，向大气中排放了大量的硫和二氧化碳，导致酸雨和温室效应。